Kiribati

Kiribati, officially the Republic of Kiribati, is a small island state in the central Pacific Ocean. Its territory consists of 33 coral atolls and reef islands, spread over a sea area of roughly 3.5 million square kilometres, but with a total land area of only about 800 square kilometres. The islands fall into three groups, the Gilbert, Phoenix and Line Islands, and the country straddles both the equator and the International Date Line. Most of the population lives on South Tarawa, and nearly all of the land lies only a few metres above sea level, which makes Kiribati one of the countries most directly exposed to sea-level rise and other effects of climate change.

Kiribati matters for several reasons beyond its small size. Its low-lying geography has made it a leading voice in international climate negotiations and in debates over how adaptation finance, human rights and sovereignty should apply to states that could become uninhabitable. Its economy depends heavily on fishing licences, public spending, aid and the earnings of seafarers abroad, and its government has built a sovereign savings fund to cushion volatility. This entry covers the physical geography and geology of the atolls, the climate and ecological systems that shape daily life, the path from early settlement through colonial rule and independence to the present constitutional republic, and the political, economic, social and cultural structures of the country. It ends with the open questions around adaptation, migration and fiscal resilience.

Name and terminology

Origin of the name

The name Kiribati is a local rendering of "Gilberts", the English plural of the Gilbert Islands, the group that forms the core of the country. The English name traces to 1788, when the British captain Thomas Gilbert crossed part of the archipelago. Around 1820 the Russian admiral Adam von Krusenstern and the French captain Louis Duperrey recorded the group as îles Gilbert. Gilbertese has no letter "s": the sound is written "ti", so "Gilberts" became "Kiribati" in the local language, pronounced roughly "ki-ri-bas".

The colonial name lasted for roughly a century and a half. The islands became a British protectorate in 1892 and joined the Gilbert and Ellice Islands Colony in 1916. "Gilbert" stayed in use as the name of the island group throughout the colonial period and the move toward self-government. Gilbertese speakers used a different name for the core chain, Tungaru, which is often cited as the indigenous name for the Gilbert Islands proper. Earlier European sources also used the name Kingsmill for the group.

Gilbertese language and the term I-Kiribati

The language is called Gilbertese, or te taetae ni Kiribati. It is an Austronesian language of the Micronesian branch of the Oceanic languages. It is spoken in a relatively uniform way across the islands, although it shows considerable borrowing from Polynesian languages. English is the official language and is taught in schools, but it is seldom used on the outer islands, where many adults speak little of it.

Citizens are called I-Kiribati. The prefix "I-" marks the people, and the same construction is used for a few other countries, which makes the demonym unusual. Older English sources also use "Gilbertese" for the people, and "I-Tungaru" appears as an alternative label that reflects the older name of the core islands.

Official name and its spelling

The state became independent on 12 July 1979 as the Republic of Kiribati, with Ribaberiki Kiribati as the Gilbertese form of its full name. The name was chosen by Chief Minister Ieremia Tabai and his cabinet. Its supporters argued that it was modern and that it covered the Phoenix and Line island groups, which were never part of the Tungaru or Gilberts chain. In a 1979 treaty of friendship, the United States relinquished its claims to the sparsely inhabited Phoenix and Line islands, which gave the country its present geographic composition. The Ellice Islands had separated earlier, in 1974, and became Tuvalu.

In English, the spelling is the same as the Gilbertese form, and the country is usually called Kiribati in short. The former name "Gilbert Islands" survives mainly as the name of the central island group and in historical references.

Island names and administrative divisions

Most islands carry Gilbertese names, such as Tarawa, Abaiang, Abemama and Tabiteuea. The local term aono ni Kiribati is used for the Gilbert group as a whole. Banaba, a raised island west of the chain, is also known as Ocean Island. Foreign place names were adapted to Gilbertese phonology: Kiritimati, the atoll known in English as Christmas Island, takes its name from "Christmas" written under the same sound rules, and it is the largest atoll in the country.

Administrative descriptions vary by source. One source describes six districts, namely Tarawa and the Phoenix group, North, South and Central Gilberts, Banaba, and the Line Islands, subdivided into 21 island councils, one for each inhabited island. Another source states that the three island groups now have no administrative function and that the districts were formally used before independence. The seats of government lie on the islets of Ambo, Bairiki and Betio on South Tarawa.

Geography and island groups

Kiribati comprises 33 islands grouped into three geographical units: the Gilbert Islands, the Phoenix Islands and the Line Islands. The Gilbert group lies on and around the equator, and in the west it includes Banaba (Ocean Island), a raised limestone island that is the only non-atoll in the country. Counts of the Gilbert atolls vary by source, with figures of 16 atolls plus Banaba and 17 islands including Banaba both in use. The Phoenix group lies about 1,800 km south-east of the Gilberts, and the Line group, which contains the country's easternmost islands, lies about 3,300 km east of them. The islands extend roughly 3,900 km from east to west and about 2,100 km from north to south, straddling both the equator and the International Date Line.

The position relative to the date line has been changed by government decision. Before 1994, the Phoenix and Line groups were on time zones several hours behind the Gilberts. In 1994 they moved forward to UTC+13 and UTC+14, and on 1 January 1995 Kiribati unilaterally moved the International Date Line eastward so that the whole country shares a single calendar day. The three groups now observe different offsets, from UTC+12 in the Gilberts to UTC+14 in the Line group, and the country does not observe daylight saving time.

The national land area is about 811 km², of which the great majority is low-lying coral atolls; most land is less than two metres above sea level. Kiribati's exclusive economic zone, the maritime zone within which the state holds sovereign rights over living and non-living natural resources, covers about 3.4 to 3.5 million km² according to the figures commonly cited, depending on the method and date used. The ratio of marine to terrestrial territory is therefore more than 4,000 to 1. This maritime domain is the basis of the country's most valuable economic sector: foreign fleets, mainly tuna fishers, pay access fees under bilateral arrangements, and the revenue has long been a central part of public finance. A very large sea area with a small, dispersed population also makes monitoring and enforcement of the zone demanding. The Phoenix Islands Protected Area, covering about 408,250 km² and roughly 11 per cent of the zone, illustrates how the maritime domain is also used for conservation. The 1979 friendship treaty with the United States, under which Washington relinquished its claims to the Phoenix and Line groups, is the reason the present territory has its current shape.

Kiritimati (Christmas Island), in the northern Line Islands, is the largest atoll in the country and one of the largest coral atolls in the world by land area. Its land area is generally given as about 312 km², with a lagoon of about 328 km², which makes it roughly 38 per cent of the national land total. Some older sources put its share at "more than half" of the country's land, reflecting earlier area measurements, so the figures should be read with care. The island's economic and demographic weight is greater than its share of land would suggest. Its population was 7,369 at the 2020 census, which is a small fraction of the national total of about 120,000, but it has grown faster than any other island in the country, rising from around 2,000 in 1989 to roughly 5,000 in the early 2000s. Kiritimati also elects three representatives to the national legislature, the Maneaba ni Maungatabu.

Most people live in the Gilbert group. Its 21 inhabited islands each have an island council, and the country is divided into six districts. Over 90 per cent of the population lives in the Gilbert chain, and more than a third of the national population is concentrated in the urban area of South Tarawa, the capital. The Phoenix and Line groups were not permanently inhabited until the twentieth century. The Phoenix group has very few residents, and Canton is its only inhabited island, with 41 residents in 2005. Earlier attempts to settle parts of the Phoenix group in the late 1930s were abandoned by 1963. Distances between island groups are large, so links between them depend on air services and shipping, and the outer islands are isolated from one another as well as from the main urban centre.

Geology and atoll formation

Kiribati's land is almost entirely coral. All the islands are low-lying coral atolls rising to no more than 3–4 m above mean sea level, with the exception of Banaba, which is a raised reef. The atoll form is usually explained by the subsidence model Charles Darwin developed during the voyage of the Beagle and published in 1842. In his sequence, reef corals first colonise the shore of a volcanic island. As the island sinks, the reef grows upward and is separated from the land by an expanding lagoon, which turns it into a barrier reef. Eventually, the volcanic island disappears beneath the ocean, leaving a ring-shaped coral reef enclosing a central lagoon.

The Gilbert Group, the largest of the three island groups, is geologically varied. It includes 11 atoll reefs and five table reefs. Table reefs are lagoonless limestone islands, and the Gilbert atolls differ from one another in how far their lagoons are enclosed. At Marakei the lagoon is almost completely enclosed, while at Nonouti and Tabiteuea there is no real constriction at all. The islands of the Gilbert Group developed on a northwest-trending series of slowly subsiding, mid-oceanic volcanoes on the western edge of the Central Pacific Basin. Magnetic anomaly dating places the underlying crust in the Early Cretaceous, about 126 million years old, near Tabiteuea and Beru, and in the Late Jurassic, about 139 million years old, further northwest near Butaritari. Kiribati's volcanic cores have never been reached by drilling. The nearest comparable boreholes, at Funafuti in Tuvalu and Enewetak in the Marshall Islands, were still in limestone at 330 m and only reached basalt beneath about 1,300 m of limestone, respectively. Volcanic activity in Kiribati is thought to have occurred between roughly 50 and 10 million years ago.

Kiribati lies on the Pacific Plate, and the long-term sinking of its islands is linked to the cooling and sinking of the oceanic crust beneath them. The crust underneath these seamounts tends to subside as it cools and thus the islands and seamounts sink. Estimates of the present rate in the Gilbert Group are small. One report suggests subsidence of about 0.05 mm per year. For Enewetak, a modelling study used an average subsidence rate of about 68 m per million years, a figure that is not Kiribati-specific but indicates the scale involved. The subsidence history is also uncertain. A new trench has been proposed southwest of the southern Gilbert Group, but its effect on present subsidence rates is not resolved.

Darwin's theory was partly confirmed by the deep drilling at Funafuti in 1896–1898. That borehole did not reach volcanic basement, passing through more than 300 m of shallow-water carbonate. Later work shows that the reef's growth did not always keep pace with the sea. On atolls, reefs often lagged behind sea level and then caught up as the rate of sea-level rise slowed. Once they reached the surface, reefs grew mainly vertically. During glacial periods, when sea level fell, reef platforms were exposed and the emergent limestone was dissolved. Rainwater dissolved exposed flat carbonate platforms into bowl-like shapes with raised edges, and corals colonising those edges raised them further. A 2022 numerical study of Enewetak supports the view that differential dissolution, weaker at the margin and stronger in the interior, is what most likely controls whether a central lagoon forms. Reef-island evidence in Kiribati also points to recent changes in sea level. The islands of the Gilbert Group are geologically very young, and appear to have developed in the last 3,000–4,000 years during a period when relative sea level has fallen.

The typical atoll islet is a narrow strip of land. The atolls like Tarawa consist of an outer rim of multiple narrow islets surrounding a lagoon. The typical atoll islet features a shallow lagoon-ward slope, an ocean-ward ridge that reaches 2–4 m above mean sea level, and a reef flat of varying widths. Individual islets are called motu, a Polynesian term widely used across the Pacific. The soils over the coral limestone are thin and poor. Kiribati's atoll soils, derived from coral limestones, are shallow, alkaline, coarse textured and lacking in nutrients. Soils on Kiritimati are weakly developed, with low organic matter and low water-retention capacity, which the study attributes to the age of the parent material and the island's relatively dry climate.

Kiritimati, the largest atoll, differs from the Gilbert atolls in its geological history. It is slightly higher, much larger and has a distinct and more diverse environment compared with the other atolls of Kiribati. Some of its lagoons are caused at least in part by uplifting, of which evidence can be seen in its landforms, and drilling data from the island have been read as evidence that the atoll has not been subsiding. The differences in foundation movement help explain why some islands are more stable than others. Where a foundation sinks slowly, as in the Gilbert Group, reef-flat sediment and reef-edge growth control whether islets widen or retreat, while uplifted islands such as Kiritimati and Banaba respond differently to waves and sea level. Coastal change is therefore shaped by both the sediment that reef organisms produce and the tectonic setting of each island.

Climate and weather patterns

Kiribati has a tropical maritime climate with very little temperature variation through the year. Air temperatures track the temperature of the surrounding ocean, and the difference between the warmest and coolest months is small, generally no more than about 1 °C. Daily temperatures usually range from about 25 °C to 32 °C. The Kiribati Meteorological Service puts Tarawa's average air temperature at 28.3 °C for 2008–2018. Humidity is high year-round, and daytime sea breezes take some of the edge off the heat, though nights can feel muggy.

Rainfall shows much more variation, both across the islands and across the seasons. Two rain-bearing systems shape it: the South Pacific Convergence Zone and the Intertropical Convergence Zone. Where converging winds lift air over warm water, thunderstorms form and heavy rain follows. In Tarawa the wet season generally runs from about November to April, while the driest six-month stretch begins in June, with the lowest mean rainfall in October. Sources disagree on the wind regime. One describes southeast trade winds from March to November, another describes northeast trade winds from April to October, and westerly winds bring the heaviest rain in the wet months. Annual totals fall from north to south: the northern Gilberts can receive around 3,000 mm, while the Line Islands are much drier. Kiritimati has its wet season from about January to June. The central Line Islands, including Malden, are semi-arid and receive only about 450 mm a year, even though they sit near the equator.

The El Niño–Southern Oscillation (ENSO) is the main source of year-to-year variability. El Niño phases tend to bring warmer and wetter conditions than normal, while La Niña phases are usually associated with suppressed rainfall and recurring drought. These episodes return roughly every two to seven years. The range in Tarawa is extreme: in the driest years only about 150 mm has fallen, while the wettest years have exceeded 4,000 mm. Notable droughts include the period from 1988 to 1989, when only about 205 mm fell, and the 2007–2009 episode, during which groundwater turned brackish and most plants yellowed. The La Niña conditions that began in late 2021 produced a severe drought. In June 2022 the government declared a state of disaster, and it reported that the whole population of about 120,000 had been affected, with the most acute conditions on Tarawa. Rainfall in South Tarawa dropped to less than a quarter of its two-year average, and the freshwater lens became markedly saltier. ENSO also affects the ocean: sea levels and sea-surface temperatures rise during El Niño events, and future changes in the frequency or intensity of these events remain uncertain.

Kiribati lies close enough to the equator to sit outside the main tropical cyclone belt, so full typhoon-strength systems rarely affect it. The islands do experience occasional gales, strong winds during the rainy season, and occasional tornadoes. Storm surges are the more damaging storm hazard. Together with prolonged droughts and episodes of extreme rainfall, these irregular events interrupt food production, contaminate or overwhelm rainwater storage, and compound the effects of seasonal dry spells. The seasonal and episodic hazards therefore converge on the same vulnerable resources, a point that the sea-level and groundwater sections develop further.

Climate records come mainly from the Kiribati Meteorological Service, which operates five stations at Tarawa, Kiritimati, Beru, Kanton and Butaritari. Its temperature and rainfall records, dating from 1947, have been analysed jointly with Australia's Bureau of Meteorology and CSIRO. Regional projects, including the Pacific Climate Change Science Program, have assembled these data together with climate model output. Observed warming in the island groups has been estimated at about 0.1–0.2 °C per decade since 1950. Maximum temperatures at Tarawa have risen by roughly 0.13–0.18 °C per decade, depending on the study. Rainfall trends are less clear. Annual rainfall at Kiritimati rose significantly between 1946 and 2013, while Tarawa shows no significant trend. Rainfall at both sites varies strongly from year to year, which makes trends hard to detect. Projections point to a warmer climate, with mid-century temperature increases of roughly 1 °C to 1.5 °C depending on emissions scenario, along with a rise in average rainfall, more extreme rain events, and a projected decline in drought frequency, although with only medium confidence. Scientists also note that the historical rainfall record for Tarawa is limited, which complicates the separation of climate change signals from natural variability.

Sea-level rise and coastal vulnerability

Observed change and mid-century projections

Sea level around Kiribati is already rising. Since 1993, data has indicated a rise of 1-4mm per year in sea level across Kiribati, and across the three island groups the increase over the three decades to 2022 has been 2 to 4 inches (5 to 11 centimeters). Projections for mid-century are comparatively narrow. Under a medium-emissions pathway the national meteorological service expects sea level to rise by 10 to 20 cm by 2050, and NASA's estimate for the islands is an additional 6 to nearly 12 inches (15 to 30 centimeters) by 2050. The uncertainty grows after mid-century. By the end of the century, depending on future greenhouse-gas emissions and the intensity of global warming, Kiribati sea level could rise by 1 ½ to more than 3 feet (50 to 100 centimeters). The unlikely but worst-case scenario approaches 2 metres.

Because the country's land rarely rises more than a few metres above the sea, small vertical changes translate into large areas of exposure. Modelling for Tarawa, the capital atoll, projects that under a best-guess scenario 18 percent of Buariki could be inundated by 2050, rising to up to 30 percent of Buariki by 2100, while the impact on Bikenibeu would be relatively minor (2 percent inundation). Other assessments use different metrics and reach stronger conclusions. One UNDP profile estimates that under the RCP2.6 scenario, almost 30 % of the population in Tarawa will be exposed to permanent inundation. Earlier studies also give a higher figure for shoreline displacement on Tarawa, by 0.2─0.4 meters by 2050, which shows how sensitive local estimates are to modelling assumptions.

Some islands have already disappeared. According to the Pacific Regional Environment Programme, two small uninhabited Kiribati islets, Tebua Tarawa and Abanuea, disappeared underwater in 1999.

Erosion, seawalls and engineered defences

On South Tarawa, erosion is linked to changes in the reef and lagoon as well as to sea level. Researchers have described the reef as the primary coastal protection structure along the ocean shoreline of the atoll and its preservation is essential. Causeways have altered this system: construction of causeways over the past few decades has closed all ocean-lagoon passages in South Tarawa, effectively eliminating water exchange along the southern boundary of the lagoon. Sand and gravel extraction has added to the problem, since sand and gravel mined for construction work has eroded beaches on Kiribati.

Seawalls are the dominant hard measure. Sea walls in Kiribati are normally built from coral rock, sand bags and concrete blocks. In a study of four South Tarawa islets, 95 percent of engineered coastal structures were seawalls. Their track record is mixed. Many were built by island councils in the late 1970s and early 1980s, and these seawalls require regular maintenance against the natural deterioration caused by wind, currents and waves. Maintenance is a persistent weakness, because expensive, hard measures require regular maintenance; which is rarely provided by international cooperation that pays for the structures. Seawalls can also shift the problem elsewhere. Research on the atoll notes that attempts to use seawalls as protective measures have had unanticipated consequences in aggravating erosion and/or diverting effects to other coastal communities.

Current measures increasingly combine engineering with nature-based work. The Kiribati Adaptation Program's initiatives include mangrove re-plantation and protection of public infrastructure. A comparative study of seawalls and mangroves found that the seawall was associated with higher perceived infrastructure protection, durability, and housing safety, while mangroves contributed more to natural capital, supporting biodiversity and ecosystems. A UNOPS project planned for South Tarawa will implement both resilient infrastructure and nature-based solutions, and South Tarawa, home to more than half of Kiribati's population, is its focus.

Storm surge and king tides

Short-term flooding often does more damage than the slow rise in mean sea level. Causeways on South Tarawa and the outer islands are flooded during exceptionally high spring tides and storms, and the national adaptation project profile observed that existing designs do not appear to be sufficiently strong against sudden storms. Modelling of the combined effect of surge and rising seas suggests much greater impacts. Under such conditions 66–100 percent of all roads lost on Tarawa, and losses would be larger in larger storm surges (such as one in 50-100 year events).

In-situ adaptation versus relocation

The government's main strategy has been to keep people on their islands. In situ adaptation is the main current strategy promoted by the Government of Kiribati. Kiribati's Migration with Dignity policy has been described as allowing individuals and families to each decide against migration, while leaving open the possibility of moving in the future. Later analyses note that the policy has been abandoned as an official government strategy, replaced instead by an approach based on economic prosperity, climate change adaptation and mitigation. As of 2017, no full-scale relocation of Kiribati's population is currently on the table.

The disagreement concerns what each option means. Advocates of in-situ adaptation argue that in situ adaptation measures would be the only ones that respect the I-Kiribati's claim to that particular territory, while those who accept migration stress that if the I-Kiribati want to relocate elsewhere, this is entirely legitimate. Cultural arguments are central. Concepts of land – with their component of people belonging to land – and ideas of the future play a significant role in these cultural logics. Research on past Pacific relocations also suggests that the cultural losses incurred when people with strongly-located cultures are forced to move are easily overlooked. Legal questions follow as well, because relocation would mostly imply leaving Kiribati, therefore, crossing of sovereign borders. Some researchers therefore argue that the two approaches are complementary, and that in situ and ex situ adaptation do not have to be alternatives to each other but both parts of a more extensive holistic adaptation policy.

Freshwater resources

Kiribati has no rivers, streams or natural lakes, so its fresh water comes from two sources: rain and the freshwater lens. The lens is a body of fresh groundwater that floats on denser seawater inside the porous coral sediments of each atoll. Rainfall that soaks into the ground is its only recharge, so its size depends on rainfall, infiltration and losses to evapotranspiration. Dense coconut plantations and thick vegetation lose more water to plants before it reaches the lens, while permeable coral sand lets water infiltrate quickly. On many islands the lens lies only a metre or two below the surface. It is thickest under the centre of wide islands and thins toward the shoreline.

On South Tarawa, the capital, piped supply comes from infiltration galleries on Bonriki and Buota. These are long horizontal pipes that skim fresh water from the top of the lens, because vertical wells can draw up the brackish water beneath it. Sources give different counts of galleries (24 in one, 28 in another). Earlier assessments put the total sustainable yield of the two lenses at about 2,010 cubic metres per day, and projected that climate change could cut the size and yield of the Bonriki and Buota lenses by around 20 per cent from about 2030. Modelling of the lens also showed how sensitive it is to rainfall: a 25 per cent fall in long-term daily rainfall was estimated to reduce average lens thickness by 64 per cent. A World Bank study concluded that the Bonriki lens could not sustain even very small pump rates during a one-in-fifty-year drought. Piped water has been rationed; at one point residents received access for only two hours every second day.

Salinisation is a second threat. Rising sea levels raise the water table and push the boundary between fresh and salt water inland and upward, which thins the lens and brings salt water toward well intakes. Storm surges and high tides can flood the islets and drive salt water into shallow pits and wells within hours. Groundwater contamination was reported as early as the late 1970s. A hydrogeological survey on Abaiang, combining resistivity imaging, infiltration tests and salinity and bacteria sampling, found that the shallow hand-dug wells common there were highly vulnerable to both salt and contamination. The IPCC's Sixth Assessment Report has estimated an 11–36 per cent reduction in fresh groundwater volume on small atoll islands due to sea-level rise. Projections for Kiribati indicate that simultaneous inundation and drought could reduce lens yield to zero for up to five years, which means the lens cannot be relied on as the main water source under continued climate change. Monitoring data from Bonriki, collected over more than three decades, have also been used to study how quickly a lens recovers after pumping and variable recharge.

Water quality on South Tarawa is closely tied to sanitation. Human and animal wastes pollute the lens, and a planning assumption held that about half of household wells would be too polluted to use. Open defecation is reportedly practised by almost half the population, and effluent leaking from pit latrines and poorly maintained septic tanks reaches groundwater. Some toilets flush with seawater through a separate reticulation system so that scarce fresh water is conserved. The health consequences are measurable. In 2010, nearly one in four people in South Tarawa was affected by diarrhoea or dysentery severe enough to require a clinic visit, and in the crowded area of Betio the proportion was 54 per cent. Infant mortality of 46 per 1,000 live births has been partly attributed to infantile diarrhoea. Between 2014 and 2016, about 80,000 cases of waterborne disease were reported in connection with deficient water supply and poor sanitation. Women and girls, who usually fetch water and care for sick family members, bear a disproportionate share of the burden.

Responses are focused on supply, storage and treatment. Rainwater tanks are widely used as a supplement, and many households in South Tarawa and most in North Tarawa also rely on household wells. The South Tarawa Water Supply Project is designed to reach around 56,000 people, about half the national population, with reliable and safe reticulated water. Its design documents describe a desalination plant and distribution network, because Tarawa's lens has become polluted and rainwater collection can only partly meet demand. Pumping from less populated islets has not kept pace with demand. Rainwater collection remains expensive on South Tarawa given its low, narrow land and limited catchment, so it is more feasible on the outer islands.

Ecosystems and biodiversity

Reefs, lagoons and seagrass

The ecosystems of Kiribati's atolls are mainly marine, and the most varied habitats lie in the lagoons and reef systems. Habitat diversity is especially high on the atolls, which include lagoon reefs, passes, reef holes, shallow reef flats, reef slopes, deeper reef terraces, mud flats and sand flats, and some settings take on estuarine traits during the wet season. Diversity declines from west to east across the central Pacific, and seagrasses, mangroves and barrier reefs become scarcer in the same direction.

Seagrass is among the least studied of these systems. Recent marine reviews have said little about seagrass, and the government has only recently started seagrass surveys within its fisheries research monitoring. Research on Tarawa Lagoon has linked seagrass to nearshore fisheries, threatened-species conservation and human health, which makes it a priority for coastal management. Government reporting presents intact reefs, fisheries and mangroves as the basis of livelihoods, health and culture, so degradation of these systems carries social as well as ecological costs.

Terrestrial vegetation

Land vegetation is sparse. Terrestrial habitats are mainly narrow coastal strands and scrub or woodland, often coconut and pandanus, along with small wetlands or mangroves where they occur. Coconut palms and pandanus tolerate salt spray and poor, sandy soils, which allows them to persist on low, narrow islets where few other plants can establish. The flora is limited in species, but it matters for wildlife and for culture, and the Phoenix Islands Protected Area still holds rare traditional plants with cultural and medicinal value that are now threatened on more populated islands.

Introduced and invasive plants have changed the landscape. Te Ango (Premna serratifolia) now dominates the South Tarawa landscape, while lantana, Singapore daisy and sweet-scent are recognised as serious threats to the natural character of the islands. Exotic plants have also been linked to harmful effects on some seabird species.

Seabirds and marine species

Seabirds are a defining feature of the outer atolls. The country supports 21 breeding seabird species, many of which are considered globally important, and two of these are threatened with extinction. Kiritimati is a stronghold for three endangered or vulnerable land and seabird species: the Phoenix Petrel, the White-throated Storm-Petrel and the Christmas Island Warbler. Seabirds also link marine and terrestrial systems, because they feed at sea and deposit nutrients on land that enrich coastal vegetation and nearshore waters.

National biodiversity inventories record 567 species of fish, 361 species of coral, 289 invertebrate species, 275 species of plants, 51 species of birds, 26 mammal species, including 20 marine mammals, and 8 species of reptiles, including the critically endangered hawksbill turtle. Counts vary by source. Figures for the Phoenix Islands alone, for example, report approximately 800 known species of fauna, including over 200 coral species, 500 fish species, 20 marine mammals and 44 bird species.

Threats

Invasive mammals are the most serious threat to the seabird colonies. Invasive alien species are regarded as the greatest global threat to seabirds, causing adult deaths and lower breeding success through predation on eggs and chicks. In Kiribati, the introduction of alien invasive species, in particular Pacific rats and cats, has substantially affected seabird breeding, and some islets have been abandoned when these predators are present.

Human pressures compound these effects. Other threats to seabirds include poaching, pollutants from commercial fishing, and the potential effects of climate change on food availability and the quality of nesting areas. On Kiritimati, population growth has increased illegal killing of adult seabirds and collection of eggs for food. Overharvesting of reef fish, invertebrates and sand for construction also depletes stocks, and this depletion is amplified on urbanized atolls, where alternatives are scarce and imports are expensive. Past military bombing, coastal construction, sewage nutrient pollution and oil spills have added to the stress on coral reefs.

Conservation responses

Rat eradication has produced measurable results. Removing rats from two Phoenix Islands islets and from many islets in the Kiritimati lagoon has improved nesting productivity and increased seabird numbers locally. In 2024 the Wildlife Conservation Unit and BirdLife International completed baiting operations to eradicate Pacific rats from 13 motu, including Motu Upua in the Kiritimati Central Lagoon. Re-invasion remains a risk: on some of these islets, rats and one cat were confirmed present again, likely following a reduction in lagoon water level.

The Phoenix Islands Protected Area (PIPA) is the largest single conservation measure. It was first declared at the 2006 Conference of the Parties to the Convention on Biological Diversity in Brazil, and formal regulations adopted in January 2008 more than doubled its original size. It covers 408,250 km², about 11.34% of Kiribati's exclusive economic zone. Within it, 3% of the protected area is closed to all fishing, and additional fishing restrictions cover a further 12.5% of the total area. PIPA is also a feeding and spawning site for tuna. Beyond PIPA, 22 Key Biodiversity Areas have been identified, covering roughly 74% of the country's land, lagoon and reef habitat. As of 2013, 12 of these 22 areas had been fully or partly established as conservation areas by the government or village communities. The national invasive species strategy for 2015–2020 is another commitment, and it addresses the threats described above.

Early settlement and traditional society

First settlement

Austronesian-speaking voyagers are generally thought to have reached the Gilbert Islands first, and sources give widely differing dates. One account puts the first settlers in the Gilberts and Banaba 4,000 to 5,000 years ago, having come from Southeast Asia by way of Micronesia. Other accounts put the first arrivals near 3000 BC, but describe the islands as not widely settled until about A.D. 200. Linguistic evidence suggests that people from southern Melanesia may have arrived well before AD 600. Physical evidence is sparse, because atoll environments preserve organic remains poorly and rising seas have eroded or submerged many coastal sites.

The Line and Phoenix groups, by contrast, had no prehistoric population. Their human history therefore begins with later contact rather than with the voyagers who settled the Gilberts.

From roughly the fourteenth century, migrants from Samoa, Tonga and Fiji arrived in the southern islands. Their influence added Polynesian elements to an existing Micronesian base, and intermarriage over time produced a population that is fairly uniform in appearance, language and customs. Language and culture still show borrowing from western Polynesia.

Navigation and canoe voyaging

The first settlers crossed open ocean in outrigger canoes, steering by stars, swells and currents. Much of what is documented about wayfinding in the wider region concerns the Marshall Islands, where navigators used stick charts. These charts were made from thin strips of coconut frond midribs or pandanus root, and small shells or coral pebbles marked islands while curved sticks represented wave patterns. The charts were not carried on a voyage; navigators studied them beforehand and then relied on the feel of the canoe and the swell. Because the charts varied so much in form, they were "readable" only by the specific navigators who constructed them. The Gilbertese record of such practices is thinner, and the detail that survives should be read as regional rather than specifically Gilbertese.

Star-based navigation was also central in the broader Pacific. Navigators memorised star sequences for each route and used a star compass, drawn in the sand with shells to represent the constellations. Knowledge of this kind declined in the colonial era. Its use in inter-island travel apparently came to demise after World War II, when travel between islands by canoe halted, and its revival elsewhere in the Pacific has been partly driven by the reconstruction of voyaging canoes.

Kin groups, land and reef rights

Atoll subsistence depended on marine resources and on a small number of cultivated crops, notably swamp taro, pandanus and coconut palms. Under these conditions, access to land, lagoon and reef was a matter of kinship. I-Kiribati society is commonly described as organised around matrilineal clans, and rights to land and to fishing grounds were held by kin groups rather than by isolated individuals. Those rights were exercised through lineage membership, and land and reef resources were managed collectively. Leadership was exercised by senior men and chiefs, and community decisions were reached through consensus in the maneaba, the communal meeting house. Colonial-era officials and researchers recorded the complexity of these arrangements; a 1961 study in the <i>Atoll Research Bulletin</i> examined land-tenure problems in the Gilbert and Ellice Islands, which shows that customary tenure remained a point of administrative concern.

Oral record and genealogy

Before European contact, the past was held in oral form. Genealogies, songs, chants and narratives carried knowledge of lineage, land and voyaging from one generation to the next. In the wider Pacific, navigators learned route sequences and wave patterns through memorisation and song, and the same mnemonic methods likely supported genealogical and territorial knowledge in the Gilberts. Because such traditions were not written down, their chronologies are shallow and often merged with ancestral and mythical elements, which makes it difficult to separate them from later additions. The modern written history of Kiribati therefore relies on archaeology, linguistics and the observations of later European visitors, with oral traditions serving as a complementary but harder-to-date source.

Colonial rule and World War II

Early contact and the labour trade

The first Europeans to lay eyes on the islands were Spanish explorers who sighted Christmas Island in 1537. Sustained contact came much later. The Gilbert Islands were a favorite whaling ground, and deserting crews began to settle on the islands in the 1830s. Trading ships were calling there regularly by the 1850s, and a flourishing copra and coconut trade was established by the 1860s, as well as an illicit human traffic.

That traffic was known as blackbirding. Blackbirders kidnapped islanders for labour in Peru and Queensland plantations, and sent Gilbert Islanders to Guatemala, Mexico and Peru to work in plantations and mines there. Outside pressure combined with new weapons and diseases. The introduction of European religious customs, diseases, and weapons disrupted native life, exacerbating conflicts among the local tribes. Historians describe this disorder as the background to London's decision to intervene.

Protectorate and the Gilbert and Ellice colony

Britain declared its protectorates in 1892, and local motives were part of the picture. One study finds that local desire for protection from potential foreign threats, particularly from France, significantly influenced the decision to declare a protectorate over the Ellice Islands in September 1892. Yet the islands were of limited value to London. Yet Britain raised the flag over the two groups at a time when her avowed policy was to avoid further colonial entanglements. Administration was handled from Fiji, as the Western Pacific High Commission had jurisdiction over the new territories.

The most valuable resource was phosphate. Britain annexed Banaba (Ocean Island) in 1900 upon discovery of valuable phosphate deposits. Mining was run by the Pacific Phosphate Company, which brought the first Japanese to Ocean Island as mechanics in 1905, and Japanese labourers were also brought from the early 1910s onwards as the company faced work problems from Gilbertese and Chinese workers. Ocean Island served as the capital from 1908 to 1942, according to the Capital: Tarawa (1895–1908 & 1946–1976) Ocean Island (1908–1942) Funafuti (1942–1946) record.

Administrative unification followed. This process started with the 10 November 1915 Order in Council making the Protectorate into the Gilbert and colony, which took effect in 1916. The Ellice representatives were "absolutely unwilling" to be ruled by the Gilbertese. Expansion continued afterwards: the Line and Phoenix Islands were incorporated piecemeal over the following two decades. Over this period the recorded population rose from 26,430 in 1892 to 33,713 in 1935 and 53,517 in 1968.

Japanese occupation and the Battle of Tarawa

The Japanese advance came quickly. The Japanese first attacked and occupied the Gilbert Islands (as they were then known) just days after their attack on Pearl Harbor in December 1941. Their interest was strategic: a remote place with little connection to the rest of the world, Kiribati offered a geographic stronghold from which Japan could bolster its empire and expand its defensive perimeter. Between 1941 and 1943 Japan turned Tarawa and Abemama into fortified places with airfields.

Occupation bore heavily on civilians. The Japanese destroyed all local boats to prevent people escaping. Gilbertese men were required to work, clearing trees and constructing gun emplacements; and when the work was complete, the entire population was forcibly moved off Betio. In October 1942, the Japanese executed 22 Coastwatchers and civilians on Tarawa, two of whom were Australians.

The Allied counteroffensive reached Tarawa in late 1943. The operation commenced on November 20, 1943, with the Second Marine Division landing on Betio, within the Tarawa Atoll, and this assault became the Battle of Tarawa. Nearly 6,400 Japanese, Koreans, and Americans died in the fighting, mostly on and around Betio. Approximately 2,000 of these men were unarmed workers, Japanese or Korean civilians, and the Japanese garrison was almost destroyed. For islanders, the physical damage lasted. Four million pounds of explosives were hurled at this island measuring about 1 square mile in size. Pictures of the battle's aftermath show the destruction it caused, which included the loss of almost every tree on the island – a loss that would have significant impact on the people of Betio in years to come.

Postwar period

The administrative centre returned to Tarawa in 1946, after wartime use of Funafuti. Many Banabans were resettled on Rabi Island in Fiji after the war, a displacement that remains part of the Banaban story. Copra remained the main commodity of the islands' trade, but prices were unstable. Through the 1920s On Chong experienced gradual decline in its operations as the result of low copra prices. Commercial power also moved toward the seat of government. Burns Philp, the trading company based in Sydney, Australia, moved to Tarawa, following the seat of political power. Colonial education and public services remained limited in scope and were concentrated on Tarawa, a pattern that continued into the independence era.

Independence and constitutional development

Separation from the Ellice Islands

The Gilbert group was administered together with the Ellice Islands as the Gilbert and Ellice Islands Colony, and the two populations were far from homogeneous. The final decades of the colony's existence were marked by tension between the majority Gilbertese and the minority Tuvaluan populations, who spoke different languages and were of Micronesian and Polynesian origin respectively. Britain had already moved the colony toward internal self-rule: a new constitution was adopted in 1967 allowing for the first general elections and self-government was granted in 1972.

The decisive step came in 1974. The result was 93% of voters in favour of separation, with a voter turnout of 88%. The administrative split took effect in stages. Sources differ on the exact dates: one account states that the Gilbert and Ellice Islands colony legally ceased to exist on 1 October 1975; on 1 January 1976, the old administration was officially separated, while another gives 1 January 1976 as the date the colony ceased to exist. The Ellice group then became Tuvalu, and the Gilbert group kept its administration as the basis for a separate state.

Independence in 1979

Constitutional preparation for the Gilbert group intensified in the late 1970s. In 1977, John Hilary Smith, British Governor of the Gilbert Islands, reunited a Constitutional Convention of 150 members. A further constitutional conference met in late 1978, and its report was tabled in the British Parliament during the debate on independence. That debate also considered amendments concerning Banaba (Ocean Island), whose people sought a separate arrangement with the new state; the final constitution reflects this, since it contains a Chapter dealing with Banaba and the Banabans.

Independence was conferred by the United Kingdom. Kiribati's independence was granted by the United Kingdom as a result of the Kiribati Independence Order 1979. The new Constitution of the Gilbert Islands as an independent Republic under the name Kiribati took effect on 12 July 1979. The country joined the Commonwealth of Nations as its 41st member on the same day.

The constitutional framework

The 1979 constitution made Kiribati a sovereign democratic republic and guaranteed fundamental rights. It created a single-chamber legislature, the Maneaba ni Maungatabu, and a presidency known as the Beretitenti. The Beretitenti combines two roles: the Beretitenti shall be the Head of State and the Head of Government. The election mechanism is indirect in its first stage. The Maneaba shall after the election of the Speaker nominate, from among members of the Maneaba, not less than three nor more than four candidates for election as Beretitenti, and no other person may be a candidate. Voters then choose among those candidates. The first holder of the office was fixed by transition rules: the first Beretitenti shall be the person who immediately before Independence Day holds the office of Chief Minister under the Constitution.

The cabinet and executive are tied to the legislature. The Constitution provides for an elected legislature, an elected president and a Cabinet responsible to the legislature, and an independent judiciary and public service. The Cabinet may include the Beritenti, not more than eight other Ministers, and the Attorney-General, and a Council of State operates alongside it. Presidential powers over legislation are limited: the Beretitenti may withhold his assent to a Bill only if he is of the opinion that the Bill, if assented to, would be inconsistent with this Constitution. Where doubt remains, the president can refer the bill to the High Court. The judiciary is structurally separate, since the Judiciary of Kiribati is independent of the executive and the legislature. The presidency also carries term limits: a person may assume office as Beretitenti after election on not more than three occasions.

Amendments and debates since independence

The constitution has been amended several times. The constitution was subsequently amended in the years 1995, 2016, and 2018. Amendment thresholds vary by subject. Ordinary changes need a two-thirds majority in the legislature, while amendments affecting the protection of fundamental rights and freedoms also requires approval by at least two-thirds majority in a referendum. Changes to the chapter on fundamental rights must therefore pass a national vote, and in that case all persons who are registered as electors for the purposes of a general election shall be entitled to vote.

Debate over the presidential process has continued. In 2020, the first presidential election since independence in which two candidates only have been nominated, which raised questions about whether the three-candidate minimum had been met. A more recent controversy concerns foreign policy. Kiribati has switched diplomatic recognition between China and Taiwan three times, with the latest in 2019. In August 2026, reporting said parliament was preparing to vote on a bill that does not mention either China or Taiwan specifically, but specifies that diplomatic relations must only be maintained with UN members or permanent observers, which would exclude Taiwan. The proposal would thus place a constitutional limit on the government's diplomatic choices, which would be a notable change to the framework set in 1979.

Government and political institutions

The unicameral legislature

Legislative power sits with the unicameral House of Assembly, known in Gilbertese as the Maneaba ni Maungatabu. Members are directly elected from the island constituencies for a four-year term, joined by a nominated representative of the Banaban community, and hold the country's legislative power, including passing laws and approving the budget. Most seats are filled through island-based constituencies, some with one member and others with several. The Rabi Council's appointee represents the former inhabitants of the island of Banaba. Polls are normally held at intervals of four years, but elections in Kiribati are held every 4 years or, earlier, after a no confidence vote. Eligibility starts at age 18, and registration requires a continuous residence of 12 months within an electoral district.

The Speaker is chosen from outside the chamber's membership. The Speaker of the Maneaba ni Maungatabu is elected by the members of the Maneaba from outside of its membership. The 2024 round ran over two rounds of voting in August. Seats won 33 for the first party and 8 for the second, which was the Tobwaan Kiribati Party and the Boutokaan Kiribati Moa party respectively, showing how concentrated the seat count had become.

The president

The president, the Beretitenti, combines the roles of head of state and head of government. The Beretitenti shall be the Head of State and the Head of Government. The selection process is indirect in its first stage. The Maneaba shall after the election of the Speaker nominate, from among members of the Maneaba, not less than three nor more than four candidates for election as Beretitenti, and no other person may be a candidate. Voters then decide between the shortlisted names. The voting public then elects the Beretitenti from among these candidates.

The 2020 contest departed from this pattern. Only two candidates were nominated, which conflicted with the requirement of at least three unless section 32(2) was read differently. A June 2020 judgment by the Chief Justice, John Muria, allowed this reading of the constitution. A person may hold the office on a limited basis, since a person may assume office as Beretitenti after election on not more than three occasions, with some exceptions for succession. The president then forms the executive. The elected Beretitenti appoints a Kauoman-ni-Beretitenti (vice-president) and up to ten other Cabinet Ministers from among the members of the Maneaba. Current office holders include Taneti Maamau as president. Parliamentary accountability operates through a different route: parliament can undo Cabinet decisions through a vote of no confidence, triggering a new election.

The judiciary and customary law

The courts are structured in three tiers. The judicial system consists of magistrates' courts, the High Court and the Kiribati Court of Appeal. The High Court handles weightier matters, and appeals relating to land, divorce, and inheritance are dealt with by the High Court's Land Division. The Court of Appeal sits in Betio and has jurisdiction to hear any civil or criminal appeals as of right from any High Court of Kiribati decision on a question of law. Judicial appointments follow a formal process. The Beretitenti, acting in accordance with the advice of the Public Service Commission, makes all judicial appointments, and amongst them, the Chief Justice, the main judge of the High Court.

Customary law operates beside the statutory system. The British introduced the legal system of common law, which has increasingly been supplemented by local and customary law. Courts must take customary law into account when considering specified matters in criminal and civil proceedings.

The judiciary has been the subject of a major dispute. Several Court of Appeal judges were suspended on 6 September 2022, which led to the 2022 Kiribati constitutional crisis. The government defended the move, citing a section of Kiribati's constitution that provides a 'check and balance' to prevent the judiciary from becoming "too powerful". Later controversy centred on the acting appointment of the Chief Justice, which caused further controversy amid a lack of perceived independence and effectively of having no functional judiciary.

Parties and local government

Political parties have existed since 1965, but Kiribati has a Westminster system two-party system, which means that there are two dominant political parties since 2020, but the political parties are not central to political life. Kiribati has an informal party system. Earlier, President Anote Tong's Boutokaan Te Koaua (Pillars of Truth, BTK) came in first with 18 seats in the August 2007 elections.

Beneath the national level, local elections are held for councils, with one council in each inhabited island and 3 councils in Tarawa. This arrangement links national politics with island-level administration, although the division of authority between the two levels is not covered in the sources used here.

Foreign relations and climate diplomacy

Membership and regional standing

The General Assembly admitted the Republic of Kiribati, the Republic of Nauru and the Kingdom of Tonga to membership in the United Nations, as the 186th, 187th and 188th Member States, respectively. Entry was completed on 14 September 1999, and it placed Kiribati among the United Nations' full members. A permanent presence in New York came later. Kiribati joined the UN in 1999, but it was not until September of 2013 that it established a mission in New York. Until then, its vote was typically cast by New Zealand in a proxy arrangement, according to one older reference.

Kiribati's regional life has centred on the Pacific Islands Forum. A UN summary counts 18 members in the forum, including Kiribati, which was founded in 1971. The country hosted a forum meeting of its own, since Kiribati hosted the Thirty-First Pacific Islands Forum in October 2000. Reference sources differ on its current standing. One encyclopedic summary describes it as a full member only until recently, while the UN listing still includes it. Other institutional ties are also recorded: Kiribati is a full member of the Commonwealth, the IMF and the World Bank.

Relations with major partners

Reference profiles name China, Australia, New Zealand, and Japan among Kiribati's key partners. The United Kingdom's historical role as colonial power is reflected mainly through Commonwealth membership. Kiribati's maritime setting places it within a zone that commentators associate with American and Australian influence, and it is thought that both island nations may use closer ties with China as a way to pressure Australia. Under President Taneti Maamau, the relationship with Beijing has become far closer, and Kiribati's president has established a very warm relationship with China, emerging as one of its strongest supporters in the region.

The 2019 switch and its aftermath

Kiribati has switched diplomatic recognition between China and Taiwan three times, with the latest in 2019. In September 2019 the decision, coming four days after Taipei severed diplomatic ties with the Solomon Islands for the same reason, left Taiwan with just 15 allies around the world. Taiwan's foreign minister attributed the move to Beijing's inducements, saying that Beijing had "seduced Kiribati to change its diplomatic ties" with promises of investment and aid. Taipei's response froze joint programmes, and Taiwanese diplomats would be withdrawn from Kiribati, whose envoys would be expected to do the same.

The financial stakes were significant. In return, Taiwan provides economic aid, infrastructure investment, and educational opportunities. Kiribati students enrolled in Taiwan also faced uncertainty about whether they could complete their studies there. In August 2026, the government moved to lock in the new position: Kiribati's parliament is set to vote on a bill that would amend its constitution to prevent future governments from switching diplomatic recognition back to Taiwan. The text does not mention either China or Taiwan specifically, but specifies that diplomatic relations must only be maintained with UN members or permanent observers, which would exclude Taiwan. Although it names neither state, analysts see it as a barrier against any future return to Taipei.

Climate diplomacy

Kiribati's climate diplomacy starts from its vulnerability. Kiribati has ratified the Paris Climate Change Agreement (2016), as recorded in the World Bank's country profile. Its membership in the small-island bloc gives its government a platform for demanding deeper emissions reductions and funding for adjustment from large emitters. The Republic of Kiribati submitted its written statement on the request for an advisory opinion contained in UN General Assembly Resolution 77/276, adopted by consensus on 29 March 2023. That statement treats rising seas as an existential problem: as a low-lying country composed of 33 atolls and reef islands—32 of which stand on average just two meters above sea level, the country faces a direct threat to its existence. It also argues that the effects of climate change that disturb Kiribati people's relationship to their ocean, land, culture and family tampers directly with their very identity.

Legal analysis has focused on attribution. Sea-level rise cannot be reduced to a single act attributable to one State. Human rights arguments have been tested before the UN Human Rights Committee. In a claim by an I-Kiribati man facing deportation from New Zealand, the Committee did not find a violation on the facts, but accepted that, without robust national and international action, climate-change impacts may in principle expose individuals to risks capable of engaging non-refoulement. Civil-society evidence submitted in 2026 likewise highlights the diverse human rights impacts of sea-level rise, with particular reference to the impacts on people living in the low-lying atoll nations of Tuvalu and Kiribati. Earlier, under President Anote Tong, the government had set out a "Migration with Dignity" approach, which recognizes that mitigation and adaptation are likely insufficient to save Kiribati.

Population and urbanization

Kiribati had 119,940 residents in the provisional count of the November 2020 census, up from 110,136 at the 2015 census. Some compilations give a slightly different national total, such as 119,438 for a 2024 census, so published figures should be checked against their vintage. Growth has been slow to moderate. The CIA World Factbook put the annual rate at 1.02% in 2023, and the population of the capital has more than tripled since independence in 1979. Growth in the capital comes mainly from in-migration, while the national rate reflects natural increase offset by emigration.

The population is young, though the sources disagree on the exact indicators. In the 2015 census, residents under 15 made up about 35% of the population, and those aged 65 and over made up under 4%. For 2023, the CIA estimated a total fertility rate of 2.18 births per woman and a median age of 26.9 years. Our World in Data reports 3.15 births per woman and a median age of 22.7 years for the same year. The gap is large enough that fertility and ageing trends should be read as provisional until census-based series are consistent.

South Tarawa, the capital, covers about 15.76 square kilometres and contains more than half of the national population. The 2020 count for the area is commonly given as 63,439, although one reference assigns the same figure to the 2018 census. Its settled area now forms a nearly continuous built-up strip from Tanaea in the northeast to Betio in the west, and it hosts most government ministries, commercial activity and schools. Between 2010 and 2015 its population rose by 12.4%. Tarawa atoll as a whole averages more than 2,000 people per square kilometre, which makes the capital one of the most densely settled places in the Pacific.

Internal migration from the outer islands is the principal driver of this concentration. Development-bank analysis identifies employment, education and health services as the main pull factors, because these are scarce or absent elsewhere in the country. Government policy has pushed in the opposite direction at times. A programme in the 1990s aimed to move about 5,000 people from South Tarawa to the outer islands, and the Copra Fund Subsidy, begun in the mid-1990s, was designed to encourage people to stay in the outer islands. Rapid growth has also led to unplanned settlement, including on water catchment land, which strains sanitation, water supply and housing, as discussed in the freshwater section.

Outer-island depopulation is uneven but persistent. The atoll of Arorae recorded 1,830 inhabitants in 1968, its highest population, and 983 in the 2020 census, the lowest figure ever recorded there. A count cited in the Arorae record found about 2,100 people identifying with the atoll living on South Tarawa, roughly twice the number resident on Arorae itself. Such figures show how kinship ties and family reunification link the capital to small islands, and how remittances and visits sustain those ties over distance.

Young people are the group most affected by the limits of the urban labour market. The national statistics office's 2019/20 household survey estimated overall unemployment at 8.6% and youth (ages 15–24) unemployment at 22.5%. An ILO factsheet citing the 2020 census gives 11% overall, 27% for youth, and 47.6% of young people not in employment, education or training. The two surveys use different definitions, which explains part of the difference. More than 60% of wage jobs are located on South Tarawa, most of them in public administration, so young people who move to the capital often find limited private-sector employment. Emigration through seafarer employment and other overseas work is another major outflow, with consequences for household composition, though reliable quantified data on its effects on family structures remain limited.

Language, religion and education

Gilbertese, known in the language as taetae ni Kiribati, is an Austronesian language of the Micronesian branch of the Oceanic languages. Before missionary contact it had no written form. The Latin script came into use in the 1860s, when the Protestant missionary Hiram Bingham Jr translated the Bible into the language. The standard orthography has marked long vowels and consonants by doubling letters since independence in 1979. Gilbertese has two main dialects, northern and southern, and the islands of Butaritari and Makin speak a variant of their own. The language is regulated by the Kiribati Language Board. Estimates of native speakers run to about 120,000, and the language is far from extinct, with most speakers using it daily.

English is the country's other official language, but its everyday use is concentrated in South Tarawa, the capital, and in government offices. Most residents of the outer islands use Gilbertese as their main language. Schooling reflects this division. Under reforms linked to the Kiribati Education Improvement Program, Gilbertese became the medium of instruction in the lower primary years, while English is used as the medium in most schools at later stages. Literacy data are dated: figures reported for 2010 indicate that about 97 per cent of residents could read Gilbertese and about 80 per cent could read English. These figures, along with the sources on which they rest, should be treated as indicative rather than current.

Christianity is the dominant religion, although the state is secular and the constitution guarantees freedom of religion. The 2020 census recorded about 58.9 per cent of the population as Catholic, 21.2 per cent as members of the Kiribati Uniting Church and 16.1 per cent as other Christians, with the Bahá'í Faith at about 2.1 per cent. Catholics are concentrated in the northern islands, while Protestants form the majority in the south. The Kiribati Uniting Church, a united Protestant body descended from the Gilbert Islands Protestant Church, was formed in 1968 as an autonomous church. Its name changed in 2014 according to church accounts, while US government reporting gives 2016. Members who rejected the change continued as the Kiribati Protestant Church. Some communities, including Arorae and Tamana, have kept a one-church tradition that dates to nineteenth-century Protestant missions. Christmas, Easter and National Gospel Day are official public holidays. Estimates of the Church of Jesus Christ of Latter-day Saints membership vary. The census put it at around 6 per cent, while the church claims a higher share.

The school system is organised into six years of primary education (Years 1–6), three years of junior secondary (Years 7–9) and four years of senior secondary (Years 10–13). A 2016 program design document counted about 23,000 students, 1,000 teachers and 126 schools. Nearly all primary and most junior secondary schools are government-run, while most senior secondary schools are operated by non-government, largely church, bodies and receive heavy state subsidies, with the government partly funding teacher salaries. This arrangement continues a historical partnership between the state and the churches: the government took over primary schooling, and the churches concentrated on secondary education. Education is free and compulsory for roughly nine years, although sources give different age ranges, ending at age fourteen or fifteen. Sources also disagree on enrolment. A five-year average cited by the Australian-funded program design document puts primary enrolment at about 78 per cent of the age group, while the Global Partnership for Education reports 79 per cent for junior secondary and 57 per cent for senior secondary. Other commentary reports higher primary figures, so the precise rates depend on the source and year.

Delivering education across a country spread over roughly 3,300 km of ocean remains difficult. Schools on small, isolated islands are expensive to maintain, and school quality and access are generally better on South Tarawa. Retention is weakest at the transition points: the design document notes that many children drop out and sometimes return, that survival rates show a marked gender disparity, and that places at secondary level are limited. Competitive examinations determine progress into senior secondary, so many students cannot continue. Post-secondary and technical training is concentrated on South Tarawa and falls under a different ministry from basic schooling. Many of the most successful graduates leave to find work overseas, which contributes to a skills drain.

Culture and traditional arts

The maneaba is the main social and political institution in the village. The Kiribati word for it points to a gathering place for the people of the land. Raising one is a collective task, and every element of the building carries both a symbolic and a practical meaning. Inside, the floor is divided into unmarked but known sitting places called boti, one for each family represented, and the senior man of each household usually speaks for his family in community discussions. Seating therefore reflects social standing. In pre-colonial times, a person's place in the maneaba depended on their role in fighting, and those who had defended the village also took the lead in performances.

Its functions go well beyond formal debate. Meetings are held there, disputes are settled, feasts are shared, and people sleep there during gatherings. Matters of political, social, economic and religious life are discussed and resolved there, led by elected male elders (unimwane), village representatives and Christian leaders. It also serves for festivities, storage and as a refuge from violence. The institution has also shaped the modern state: the national legislature, the Maneaba ni Maungatabu, takes its name from this traditional meeting house, and Christianity has made the maneaba a central place of worship as well.

Music and dance are closely tied to ceremony, feasting and competition. Kiribati folk music is generally based on chanting or other forms of vocalizing, accompanied by body percussion. Traditional songs are often love-themed, but there are also competitive, religious, children's, patriotic, war and wedding songs. Public performances today usually involve a seated chorus with a guitar, but in formal dances such as the standing Te Kaimatoa or the hip-focused Te Buki, a wooden box is struck simultaneously by a chorus of men sitting around it, producing a hollow, reverberating tone.

The dance repertoire is varied. The ruoia series is among the oldest forms, with dancers moving in time with singers standing behind them. The most widely practised dance in contemporary Kiribati is the Kaimatoa, literally meaning the dance of strength. It tests physical endurance, particularly the ability to hold the arms outstretched for long periods, as well as emotional endurance. It can be performed by men, women and children. Many movements imitate the frigate bird, which also appears on the national flag. The bird is also a symbol of practical knowledge: it is said to guide lost fishermen, to give weather information, and to signify peace and harmony. The stick dance tirere is performed only during major festivals. Composition has also changed: in contemporary Kiribati almost anyone can compose a song, whereas formerly specific individuals known as te kainikamaen were responsible for creating music.

Oral tradition is the other main pillar of cultural memory. Chants and genealogies carried history across generations without writing, and navigators carried knowledge of stars and swells that guided canoes between the scattered reefs. Historical narratives and genealogies were recited by elders for centuries, and were set down early in the twentieth century by scholars and by I-Kiribati writers themselves, which gives the country one of the better documented oral bodies of tradition in the Pacific. Navigation teaching also used material aids, including stick charts (meddo), which are cited as woven pandanus maps that depict swells, islands and stars.

Efforts to protect these practices now span documentation, international recognition and climate-related planning. Kiribati deposited its instrument of ratification of the UNESCO intangible heritage convention in 2017, and the convention took effect for the country on 2 April 2018. The safeguarding work covers oral traditions, performing arts, social practices and rituals, knowledge of nature and the universe, and traditional craftsmanship. Capacity-building workshops have addressed community-based inventorying, the development of safeguarding plans, and the challenges posed by climate change. Earlier documentation has also helped preserve the repertoire: in 1963 the ethnographer Gerd Koch filmed dances on several islands, leaving a valuable audiovisual archive of Kiribati dance. Preservation faces other pressures, including the legacy of colonial exploitation, which left many objects relating to Kiribati's cultural heritage in overseas collections. The land that holds this memory is itself at risk from rising seas, which makes documenting and maintaining these practices a time-sensitive task.

Economy and labour

Fisheries and licensing

Fisheries are the country's central economic sector, but most of the value is captured through licensing rather than harvesting. Industrial-scale commercial fishing activities in Kiribati are currently exclusively oceanic and are conducted almost entirely by foreign interests. As a result of these numerous agreements and arrangements, hundreds of foreign purse seine and longline vessels fish offshore in Kiribati waters every year. The waters at issue are extensive, with the zone reaching 3.6 million square kilometers, which is why the exclusive economic zone is central to the revenue model.

Access payments have become the state's main revenue source. Between 2018 and 2022, fishing license revenues remained a cornerstone of Kiribati's economy, consistently contributing over 70% of total government income. Purse seiners carry much of this weight: they provide over 60% of fishing access fee revenue. Revenue is vulnerable to policy choices. The 2015 closure of the Phoenix Islands Protected Area to commercial fishing produced revenue losses that have been estimated at between USD 60 million and USD 140 million over the subsequent years. Accounting treatment also matters for national statistics: because the foreign fishing fleets do not establish a base of operations in Kiribati and are consequently treated as non-residents. their payments do not add to domestic output, although they raise national income measures; one estimate puts fishing license revenues, income from a trust fund, and seafarers' remittances at a level that lifts GNP well above GDP.

Domestic fishing is small-scale. Artisanal catches for household use and local sale are concentrated where demand is highest: small-scale commercial fishing is concentrated around Tarawa where a sizeable population, some ice and cold store facilities, and a cash-oriented economy create better market conditions. Ice production on the outer islands has since allowed increasing small-scale commercial landings at non-Tarawa locations.

Copra and the subsidy

Copra, the dried meat of the coconut, is the main export of the outer islands. Between 2010 and 2021, copra and broader coconut products on average accounted for 8 percent and 45 percent of Kiribati's exports, respectively. Participation is wide: around 40 percent of households produce copra for the purpose of sale or exchange, with the highest participation (up to 87 percent of households) occurring in the outer islands.

The government has intervened in prices since the mid-1990s. The subsidy takes the form of a minimum support price, guaranteeing farmers a fixed price per kilogram of copra sold. The price was raised repeatedly; the support price was doubled to AUD 4/kg in 2022, consuming 8 percent of GDP and pushing the domestic price far above regional and international market prices. The scheme serves several purposes: it redistributes fishing revenue to the outer islands, serves as an unemployment benefit for individuals who have experienced job loss, and is a type of conditional cash transfer program aimed at curbing migration from the outer islands to Tarawa. The Government's fiscal position is affected accordingly. An IMF technical assistance mission estimates that subsidies in 2023 amounted to 7.8 percent of GDP. Official budget outlays have since remained high: the copra subsidy reached about 9 per cent of GDP in 2025 and is budgeted at A$30 million in 2027. Analysts conclude that the scheme is costly and poorly targeted. They find that the copra subsidy does reduce poverty, but becomes less effective the larger it grows, and that cash transfers targeted at poor outer-island households would deliver more poverty reduction per dollar.

Seafarers and remittances

Seafaring is the other major source of cash income. Overseas employment is one of few employment alternatives for the working age population in Kiribati. Earnings sent home are a significant income component for the Kiribati economy, with immediate benefits for families and communities. In a comparison of Pacific economies, the IMF noted that Kiribati, with remittances of 18 percent of GDP, also has large receipts, mainly from earnings by seamen on foreign ships who have attended the local Marine Training Institute, which was established with donor aid in the 1970s.

Estimates of the size of the seafaring workforce differ. One source reports around 4000 trained seamen although only a minority have jobs. Another states that about 1,400 I-Kiribati are trained, certified, and active as seafarers. Remittances are sensitive to global shipping cycles: remittances dropped significantly as ships were withdrawn from service. The Support Fund for the Unemployed, which pays benefits to jobless workers, peaked at A$27 million during the pandemic, when remittances fell and supply chains broke down, and has settled at A$23 million.

Growth, prices and public spending

The economy relies heavily on income from abroad and on imports. Given Kiribati's limited domestic production ability, it must import nearly all of its essential foodstuffs and manufactured items, and the country runs a substantial trade deficit. Output growth has lagged demographic change: economic growth has been much slower than population growth since 2002, and is projected to remain so for the foreseeable future. The public sector is the largest employer, and government recurrent and development expenditures are a main determinant of aggregate demand. Private investment remains limited, so public spending and transfers are the main drivers of activity in the economy. The copra subsidy also feeds into consumer prices, since it keeps local copra prices well above world levels. Recent expansion has therefore been closely tied to government spending and to the redistribution of fishing revenue, rather than to a broad private sector.

Public finance and the Revenue Equalization Reserve Fund

The Revenue Equalization Reserve Fund

The Revenue Equalization Reserve Fund (RERF) is the country's main sovereign savings vehicle. A sovereign wealth fund financed by phosphate earnings was established in 1956. In later decades the flow of money into the fund depended largely on foreign fishing access. The IMF notes that historical fiscal surpluses were driven by robust fishing license fees, and when fishing revenue fell, the fund's inflows fell with it. In 2008, the Revenue Equalization Reserve Fund was valued at US$ 400 million. The 2008 financial crisis then reduced its value, as failed Icelandic banks and withdrawals made by the government to finance budgetary shortfalls both cut into the balance.

The fund's rules have changed several times. The 2020 budget proposed a drawdown rule under which the fund would keep its real value and grow by at least 5 percent after inflation, with any excess over this real growth rate available for infrastructure programmes. In 2024 the rule was loosened: the new rule allows withdrawals of excess annual returns above a 2 percent nominal threshold, replacing a much stricter test. Under the new rule, the 2024 RERF withdrawal was AUD 80 million, around 17 percent of GDP. Government figures released in 2025 indicated that cumulative withdrawals since 2016 were a modest 7% of the fund's total value, equivalent to $120 million, although the fund's overall value had grown to about US$1.67 billion.

Deficits, withdrawals and their sustainability

Recurrent spending has far outpaced domestic revenue. The IMF reports that this was driven by declining fishing revenues as well as an expansion of social benefits and civil servants' wage increases. The government also increased its copra subsidy, which rose from 6 to 9 percent of GDP, a change partly offset by higher excise tax collection. The gap is financed by drawing on the fund. For 2025, the IMF estimated that the overall deficit at 14 percent of GDP was financed by withdrawals from the Revenue Equalization Reserve Fund (RERF). The budget for 2026 anticipated a withdrawal of 8.6 percent of GDP in 2026.

The IMF argues that this pattern is only sustainable with a stronger framework. It recommends amending the RERF withdrawal rule to a balance-based rule so that withdrawals remain possible in years of low returns, along with integrating fund operations into a medium-term fiscal plan. It also calls for a fiscal consolidation to allow additional, more efficient, climate adaptation investment while ensuring debt sustainability. Earlier the government had reduced the deficit through a freeze on nominal wages and streamlining of subsidies.

Public debt and contingent liabilities

Direct public debt is low by regional standards but its risk profile is not. Public debt stood at 12 percent of GDP at end-2023, mainly composed of external debt to the Asian Development Bank (ADB) and Taiwan Province of China. By the end of 2025, public debt fell to 8 percent of GDP in 2025 and is assessed as sustainable, but the risk of debt distress is considered high due to long-term climate-related vulnerabilities. The IMF attributes the high risk rating mainly to climate-related vulnerabilities and implicit contingent liabilities. A significant part of the latter comes from state-linked joint ventures: Joint Venture entities with minority government ownership disclosed external debt of about 190 percent of GDP accumulated since 2019, for which the authorities report no explicit guarantees. Debt analyses have also been extended to a longer horizon, with the 2024 assessment using a projection horizon extended to 20 years to capture the impact of climate change on debt dynamics.

Fuel and electricity tariffs, subsidies and public enterprises

Electricity is a major fiscal pressure point because imported diesel is costly. The Public Utilities Board (PUB) has struggled financially: electricity tariffs for household consumers do not currently recover the costs of generation, and the utility recorded operating losses in each year from 2008 to 2017 except 2016. The government provides subsidy to the PUB equivalent to about 10% of total revenues. Fuel remained the largest cost, with its share decreasing steadily from 63% of total expenditure in 2015 to 50% in 2019. Residential tariffs were kept largely unchanged for years; electricity tariffs have been constant since 2010. The IMF later reported that inflation rose to around 6.5 percent in 2025 following long-overdue and welcome fuel and electricity tariff reforms.

Structural reform of the utilities has been proposed. The Kiribati Utilities Services Reform Programme recommended its separation into two new state-owned enterprises: "Kiribati Power" to manage electricity generation and transmission, and "Kiribati Water and Sewerage". The IMF has also stressed that it is essential to place state-owned enterprises on a sustainable footing, since their losses are a contingent liability for the budget. Higher fuel and shipping costs linked to the Middle East war have added renewed pressure on the fiscal position in 2026.

Infrastructure and energy

Transport links

Transport in Kiribati is shaped by the dispersal of its islands. The system consists mainly of short road networks on the larger atolls, domestic and international air services, and coastal and inter-island shipping, with Tarawa and Kiritimati serving as the main hubs and no railways at all. Road transport is confined to local use between villages, where privately owned small trucks and pickups carry goods, while inter-island travel relies on small ferries and outboard boats. Sea services are tide-dependent and frequently irregular, so schedules shift often.

Domestic flights are the most reliable link to the outer islands. Air Kiribati, which operates under the government's commercial arm, is based at Bonriki International Airport on Tarawa and serves destinations across the Gilbert Islands. Its cargo service runs to 16 domestic destinations, but the Phoenix and Line Islands are not served by the domestic carriers, and Cassidy International Airport on Kiritimati is the only airport in those groups reached by an airline. International flights are limited. Fiji Airways flies to Bonriki from Nadi twice a week, and the Kiribati Ports Authority runs the main ports at Betio on Tarawa and Navy Harbour on Kiritimati. Freight usually reaches Tarawa or Kiritimati first and is then transhipped to outer islands by locally owned lines, and the state-run Kiribati Shipping Services carries much of the intra-island freight.

Electricity generation

Electricity is one of the country's most fuel-dependent sectors. Oil and gas products supply about 94 percent of national energy, with the rest coming from biomass, and the Public Utility Board, a government-owned body, runs the diesel-based grid on South Tarawa. In 2012, about half of all imported fuel was burned for power on that grid, which served roughly 52,000 people. Outer islands rely on a patchwork of small diesel generators, PV-diesel micro-grids and solar home systems, and the Kiribati Solar Energy Company, which was formed in 1984 by a non-governmental organisation and is now wholly government-owned, supplies many of the latter. Solar power has grown from a small base. A World Bank-supported grid-connected project unveiled 548 kW of panels in 2016, and its developers expected to reduce diesel use by about 230,000 litres a year. A larger 7.5 MW project by the Asian Development Bank, sited on the Bonriki water reserve and paired with battery storage, is designed to power more than 9,000 homes in South Tarawa. Integrating variable solar output into a diesel-based grid requires dedicated reserves and changed operating practices at the utility, and private rooftop systems are permitted to connect only with the utility's approval.

Telecommunications and internet

For many years, international connectivity depended almost entirely on satellite links, which brought delays and unstable connections. The East Micronesia Cable System, a submarine cable of about 2,250 km, runs from Tarawa to Nauru and then through Kosrae to Pohnpei. It was funded through grants from Australia, Japan and the United States and was owned by a consortium that includes the Kiribati state telecommunications company BwebwerikiNet. NEC announced in 2026 that construction had been completed. A separate link from Kiritimati to the Southern Cross cable system, supported by an Asian Development Bank grant of $21.6 million, reduces the island's reliance on satellite. Fixed-line telephony remains limited largely to urban Tarawa, and mobile networks are the main means of access elsewhere. Vodafone Kiribati, formerly Amalgamated Telecom Holdings Kiribati, is the principal provider. Because the cable lands on Tarawa and not on the outer islands, the gap between urban Tarawa and the outer islands in connection quality and cost is likely to persist without further domestic network investment, which is still being developed.

Development partner projects

Most major projects are financed by external partners. The Australian aid investment agency's submarine-cable project is valued at about AUD 135 million and is funded entirely through grants, and the cable was jointly financed by Australia, Japan and the United States. The South Tarawa water supply and renewable energy projects were co-financed by the World Bank, the Green Climate Fund and the New Zealand government. Asian Development Bank, Australian and New Zealand support also underpins broader improvements to facilities in Tarawa and the outer islands. Coastal protection works are funded through similar partnerships, which are discussed in the section on sea-level rise and coastal vulnerability.

Health services and public health

Kiribati's health care is delivered almost entirely by the state. The government is the sole provider of health services and they are free, and there is no private health care sector. A few services are the exception: most health services are free, but some, such as dental, x-ray and laboratory services, are charged. The system is therefore a single public network, and its shape is set largely by the distances between islands.

Facility network and referral pathways

Care is organised in tiers. The national referral hospital, Tungaru Central Hospital at Nawerewere on South Tarawa, has the most specialised services. Three other referral hospitals serve other regions: one at Betio on Tarawa, one on Kiritimati for the Line and Phoenix Island Groups, and one on Tabiteuea North for the southern Gilbert Islands. On the outer islands, each island normally has a health centre run by a medical assistant, and smaller clinics are staffed by public health nurses. The number of clinics depends on population and isolation, and an integrated medical outreach team visits twice a year.

Published facility counts vary between sources. One report gives 115 health facilities across the three archipelagos, while another cites approximately 85 health centres and clinics on the Outer Islands plus the South Tarawa facilities. Many outer-island facilities are weakly equipped: most lack power and have limited means of communication, and many are staffed by a single nurse.

Referral from the outer islands depends on transport. Cases beyond primary care are sent to Tarawa via a two- to four-hour boat trip or a flight that leaves once or twice a week. Serious cases that cannot be treated in Kiribati may be sent overseas, but due to high referral costs overseas treatment is rationed by a committee of doctors and only those with a good prognosis are sent overseas.

Disease burden

Kiribati faces what international health agencies describe as a combined burden. It has the highest prevalence of communicable diseases such as tuberculosis and leprosy in the Pacific, the second highest prevalence of non-communicable diseases among the world's low-middle income countries, and some of the highest diabetes and infant mortality rates in the region. A case–control study found that the diabetes prevalence in tuberculosis cases (37%) was significantly greater than in controls (19%).

Diabetes and hypertension are the most prominent non-communicable conditions, though estimates differ by method. A nationwide survey across 21 islands reported that 38.5% of adults had hypertension (stage 2 or hypertensive crisis) and 16.5% had diabetes. The International Diabetes Federation's modelling gives a higher age-standardised prevalence, with the country in the top ten countries with the highest prevalence of diabetes (20-79 years) in the world. Gestational diabetes is also a concern, with very high rates that put many pregnancies at high risk.

Nutrition and food security

Under- and over-nutrition exist side by side. Results reveal high prevalence of overweight and obesity (78.6% in adults), alongside persistent undernutrition in children (23.9% stunting, 6.9% wasting in under-fives). Obesity is especially common among women. 53.7% of adult women and 45.4% of adult men are living with obesity.

The food system explains much of this pattern. Local food production is limited, and imported food has become the main source of diet. One health worker notes that it's difficult to grow fruit and vegetables here and accessing healthy, nutritious food is not easy. Most food is imported, and it's high in fat and sugar. Poverty, crowding and the spread of Western-style diets are cited as contributors to these health outcomes.

Workforce and delivery capacity

Staffing is the main constraint on the system. The national total in one assessment is a health workforce of 59 doctors and 385 nurses, which is small for the population spread across dispersed islands. Nurses and medical assistants carry much of the outer-island load, and a medical assistant is a nurse with additional training in medical conditions and treatment pathways who can treat patients with the support of trained physicians. On Abaiang, one medical assistant has been the sole medical assistant for six years, serving a community of 6,000 people with limited resources.

Staff loss adds to these shortages. Officials reported that over the last 12 months 30 of Kiribati's most experienced nurses left to jobs in Australia and New Zealand, and many of its doctors have also migrated to other countries. Supply and transport problems compound the difficulty, since many outer islands rely on infrequent boat or air transport for critical supplies, and delays can lead to medicine shortages and limited health care access. In response, the country launched a national emergency medical team in 2022, which has in place a national EMT capable of mounting a self-sufficient national clinical and public health response to a wide range of hazards, including disease outbreaks and disasters.

Future prospects and open questions

Adaptation finance is the most immediate constraint. Seawalls, desalination plants and the relocation of roads and housing all draw on a state budget with few domestic revenue sources. Options discussed in the wider climate policy debate include sending money directly to national and community bodies, simplifying accreditation for small states, and shifting from project-by-project grants toward budget support. Frontline communities on the outer islands are often the last to see projects approved in distant capitals.

The fiscal side of adaptation depends heavily on the Revenue Equalization Reserve Fund (RERF). The economy's narrow export base, built mainly on tuna and copra, leaves public finances reliant on fishing licence income and development partners (A narrow production and export base (mainly related to tuna fishing and copra) makes the country highly dependent on fishing license revenues and support from development partners for infrastructure investment.). The fund's origins lie in phosphate income from Banaba, which seeded it in 1956 (Kiribati has a sovereign wealth fund—the Revenue Equalization Reserve Fund (RERF)—which was established in 1956 from phosphate mining proceeds. Mining ceased in 1979 and, in recent years, fishing revenues have been used to replenish the fund.). Its balance reached about AUD 1.5 billion at the end of 2024, close to 324 percent of GDP (The RERF's balance was about AUD 1.5 billion (close to 324 percent of GDP) at end-2024.). Official commentary later reported the fund at A$1.74 billion by July 2026, and authorities cut annual dividend withdrawals from A$78 million to A$45 million to protect its real value (To protect its real value, we have reduced annual dividend withdrawals from A$78 million to A$45 million.).

The IMF's assessment highlights the risks of this model. Its revenues are volatile, which makes the economy behave more like a resource exporter than a typical small state (Kiribati relies on highly volatile revenues, akin to resource-rich economies.). Drawing on the fund in line with annual returns can amplify those swings (Domestically, greater reliance on RERF withdrawals that are based on annual returns can exacerbate existing revenue volatility and hamper economic management.). IMF calculations suggest a 5 percent balance rule would allow medium-term withdrawals of roughly 15 percent of output while keeping the fund's real value intact over the long run (With a balance rule of 5 percent of RERF, the maximum withdrawals would likely be around 15 percent of GDP over the medium term, providing substantial fiscal buffer for potential revenue shortfalls. Finally, even with the maximum annual withdrawals under a 5 percent balance rule, the value of the RERF would be preserved over the long term.). Whether that rule can survive repeated climate shocks, which also hit revenue and public spending, is an open question.

Relocation is the most contested issue. Former president Anote Tong promoted "migrating with dignity" as a policy that would let citizens move on their own terms, mainly for work abroad in countries such as Australia and New Zealand, rather than in an emergency (This policy was designed to give citizens the tools to relocate legally, finding work in other nations like Australia and New Zealand. Tong prefers this slow and methodical transition to the alternative – moving tens of thousands of citizens at once in response to a catastrophic flood or drought.). A human rights study finds that this scheme is no longer official strategy, with policy now centred on prosperity, adaptation and mitigation (Kiribati's historical 'Migration With Dignity' (MWD) relocation scheme has been abandoned as an official government strategy, replaced instead by an approach based on economic prosperity, climate change adaptation and mitigation.). A national labour migration policy, by contrast, still presents permanent relocation of some citizens as part of long-term adaptation (The permanent relocation of some of its citizens is part of the Government's long-term climate change adaption strategy.). The sources therefore diverge on how far relocation remains official policy. Under the current administration, the government has stated that people should stay (But Maamau now plans for his people to stay.).

The land purchase in Fiji illustrates the tension. Reports put the holding at roughly 20 to 22 square kilometres on Vanua Levu (In 2014, Kiribati president, Anote Tong purchased 20 square kilometers on Vanua Levu, a Fiji island making this the first international land purchase intended for climate refugees.; In 2012 Kiribati purchased 22 square kilometres of land in nearby Fiji, which is less susceptible than Kiribati to rising sea levels due to its more elevated terrain.). The land is currently used for farming (The country's land in Fiji is being used as farmland for now, though, and Kiribati faces an uncertain future.). Analysts argue that moving to another island state would leave the underlying exposure in place (But even a move to other island nations—like Fiji—won't free Kiribati from the risks of climate change.).

Legal status remains unsettled. The term "climate refugee" is associated with the case of I-Kiribati citizen Ioane Teitiota, who took his asylum claim against New Zealand to the UN Human Rights Committee after authorities had refused it (The term "climate refugees'' originates from a headline-making lawsuit surrounding I-Kiribati Ioane Teitiota. Mr. Teitiota brought a case against the government of New Zealand at the UN Human Rights Committee (HRC) in February 2016 after authorities denied his claim of asylum as a "climate refugee."). Existing refugee frameworks generally require a high level of distress before protection applies (Under existing frameworks, a certain threshold in distress would be required before I-Kiribati would meet refugee requirements.), which is poorly suited to planned, pre-emptive movement. Tuvalu's treaty with Australia offers one model of a planned mobility pathway (Tuvalu stands out as the first state to conclude a climate relocation treaty with Australia, establishing a human mobility pathway for its citizens.).

Sovereignty raises a separate set of questions. The country's 811 square kilometres of land sit within an exclusive economic zone of about 3.44 million square kilometres (Kiribati consists of 32 atolls and one island in an expanse of ocean equivalent in size to the contiguous United States.). Its maritime zones are measured from baselines, and it has set maritime boundaries with several neighbours (Consistent with the relevant provisions of the LOS Convention, the breadths of these maritime zones are measured from the baselines of Kiribati.). If coastlines recede or are submerged, the legal basis for those baselines and the zones built on them would need to be re-examined. Scholars have noted that as sea levels rise, islands are expected to lose territory, which makes relocation harder (As sea levels rise, islands are expected to see a net loss of territory over already small regions, making relocation even more difficult.). Some Pacific states have responded by publicising their maritime baselines (There is also a growing trend among Pacific island states of publicizing and declaring their maritime baselines.). Analysts link these issues to whether the nation can continue as a state if its land becomes uninhabitable (Tuvalu's and Kiribati's plans for relocation introduce new challenges for international relations and security, particularly concerning state sovereignty and the continuity of nation when their countries' land becomes uninhabitable.). Cultural continuity adds a further dimension, since Pacific islanders' identities are very much tied to their ancestral land, the physical islands on which they live. Migration may mean a national and cultural loss, especially when most traditions are preserved orally.

References

1. Kiribatibritannica.com
2. Gilbert Islandsbritannica.com
3. Kiribatidlab.epfl.ch
4. Kiribatiencyclopedia.com
5. Kiribati - Wikiwandwikiwand.com
6. I-Kiribatiethnicity.fandom.com
7. Kiribati Historical Geography • FamilySearchfamilysearch.org
8. Kiribati Country Informationaardy.com
9. Kiribati - Country Profileopenfactbook.org
10. Culture of Kiribati - history, people, clothing, traditions, women, beliefs, food, customs, familyeveryculture.com
11. Te taetae ni Kiribati - Kiribati Language Lessons - Glossarytrussel.com
12. The Nation of Kiribatieverything-everywhere.com
13. Kiribatifao.org
14. Time in Kiribatien.wikipedia.org
15. Geography of Kiribatien.wikipedia.org
16. Kiribati Maps & Facts - World Atlasworldatlas.com
17. Geography of Kiribati: Data, Topography, Islandsioa.factsanddetails.com
18. Kiribatinationsencyclopedia.com
19. 9 Kiribati in: Pacific Island Economies - IMF eLibraryelibrary.imf.org
20. Marine Atlas: Maximizing Benefits for Kiribatigrida.no
21. Kiribati - Lowy Institute Pacific Aid Mappacificaidmap.lowyinstitute.org
22. The Kiribati economy - performance and prospectsopenresearch-repository.anu.edu.au
23. Phoenix Islands Protected Areaen.wikipedia.org
24. Kiritimatien.wikipedia.org
25. Kiritimati - Wikidatawikidata.org
26. Line & Phoenix Group (Kiribati): Islands & Major Villages - Population Statistics, Maps, Charts, Weather and Web Informationcitypopulation.de
27. Kiritimati - Wikiwandwikiwand.com
28. Demographics of Kiribatien.wikipedia.org
29. Kiritimati - Island - geo.wikisort.orggeo.wikisort.org
30. Theories of Atoll Formation - Coral Reefs Part 3trtomsgeoinsights.com
31. COASTAL EROSION PROBLEMS IN THE GILBERT ISLANDS GROUP REPUBLIC OF KIRIBATIresearch.fit.edu
32. Limaloken.wikipedia.org
33. Reef-island topography and the vulnerability of atolls to sea-level riseftp.soest.hawaii.edu
34. Rethinking Darwin's Theory of Atoll Formation - Eos.orgeos.org
35. Profile of a typical Kiribati atoll islet (not to scale)researchgate.net
36. (PDF) Flora of Kiritimati (Christmas) Atoll, Northern Line Islands, Republic of Kiribatiresearchgate.net
37. The Formation of Atolls: New Insights From Numerical Simulations - Liu - 2022 - Journal of Geophysical Research: Earth Surface - Wiley Online Libraryagupubs.onlinelibrary.wiley.com
38. Atollen.wikipedia.org
39. 397 The Soils of Kiritimati (Christmas) Island, Kiribati, Central Pacific:scholarspace.manoa.hawaii.edu
40. Kiribatiebsco.com
41. Climate - Kiribati - average, annual, temperaturenationsencyclopedia.com
42. Current and future climate of Kiribati North Pacific Ocean South Pacific Oceanpacificclimatechange.net
43. Current and future climate of Kiribati North Pacific Ocean South Pacific Oceanpacificclimatechangescience.org
44. NAP-Kiribati-2020.pdfunfccc.int
45. KIRIBATI - Climate Change Knowledge Portalclimateknowledgeportal.worldbank.org
46. Kiribati - Country Overviewclimateknowledgeportal.worldbank.org
47. Kiribatipacificclimatechange.net
48. Marine water quality of a densely populated Pacific atoll (Tarawa, Kiribati): Cumulative pressures and resulting impacts on ecosystem and human health - ScienceDirectsciencedirect.com
49. Pacific: Drought - May 2022reliefweb.int
50. Kiribati Drought — AHPahp1.squarespace.com
51. El Niño's impact is being felt across Pacificpmn.co.nz
52. Annex 1 Climate Risk Profile for Kiribati Report Prepared by John E. Haysprep.org
53. 19 Chapter 4 Impact of Climate Change on Low Islands The Tarawa Atoll, Kiribatiresearch.fit.edu
54. Kiribati climate: temperature, rain, when to go - Climates to Travelclimatestotravel.com
55. Kiribati risks becoming the first country to lose its land territoryecohubmap.com
56. NASA Sea Level Team Examines an Island Nation at Risksealevel.nasa.gov
57. 19 Chapter 4 Impact of Climate Change on Low Islands The Tarawa Atoll, Kiribatimfed.gov.ki
58. KIRIBATI CLIMATE SECURITY RISK ASSESSMENT PROFILEundp.org
59. (PDF) Coastal Erosion in South Tarawa, Kiribatiresearchgate.net
60. Zoom - Protecting South Tarawa’s beaches from erosionspc.int
61. The Case of Sea Walls — Social Geography of Coastal and Marine Areasmarinesocialscience.uni-kiel.de
62. Exposure of atoll population to coastal erosion and flooding: A South Tarawa assessment, Kiribatiresearchgate.net
63. KIRIBATI: NAPA PROJECT PROFILE 1. Water Resource Adaptation Project Page 2unfccc.int
64. Kiribati Adaptation Programen.wikipedia.org
65. Coastal protection structures in Tarawa Atoll, Republic of Kiribatiresearchgate.net
66. Forging coastal resilience in Kiribatiunops.org
67. Not Just ‘Sinking Islands’: Climate Change and Adaptation in Small Island Developing States - Virginia De Biasio, 2025journals.sagepub.com
68. No Retreat: Climate Change and Voluntary Immobility in the Pacific Islandsmigrationpolicy.org
69. Migration and dignitytandfonline.com
70. An Island Nation Turns Away from Climate Migration, Despite Rising Seas - Inside Climate Newsinsideclimatenews.org
71. Directions in dealing with climate change in Kiribatipdfs.semanticscholar.org
72. (PDF) Climate Change and the Imagining of Migration: Emerging Discourses on Kiribati's Land Purchase in Fijiresearchgate.net
73. Analysis of the Challenges of a Hybrid Adaptation Policy ...earthrefuge.org
74. Kiribatiaksik.org
75. (PDF) Adaptation and the question of migration: Directions in dealing with climate change in Kiribatiresearchgate.net
76. Tackling environmental threats on Pacific atollsopenresearch-repository.anu.edu.au
77. Case Study A VULNERABILITY OF FRESHWATER LENS ON ...pacificwater.org
78. FP091: South Tarawa Water Supply Projectgreenclimate.fund
79. South Tarawa Water Supply Projectfraserthomas.co.nz
80. On the resilience of small-island freshwater lenses: Evidence of the long-term impacts of groundwater abstraction on Bonriki Island, Kiribati - ScienceDirectsciencedirect.com
81. Water Management in Kiribati With Special Emphasis On ...pacificwater.org
82. Government of the Republic of Kiribati Tarawa Water Master Plan:theprif.org
83. 49453-002: South Tarawa Water Supply Projectadb.org
84. Water Scarcity in Kiribati: Living on the Freshwater Lensfarandawayadventures.com
85. South Tarawa Water Supply Projectlivelearn.org
86. SOUTH TARAWA WATER AND SANITATION ROADMAP 2011theprif.org
87. Kiribati: South Tarawa Sanitation Project (P176478)documents1.worldbank.org
88. 43072-013: South Tarawa Sanitation Improvement Sector Project (formerly Tarawa Sanitation Improvement Project)adb.org
89. Co-designing water sanitation and hygiene (WASH) messages for a social and behaviour change campaign in Kiribati - ScienceDirectsciencedirect.com
90. 1 Environmental and Social Impact Assessment South Tarawa Sanitationdocuments1.worldbank.org
91. The World Bank South Tarawa Sanitation Project (P176478) Jun 28, 2021documents1.worldbank.org
92. Water and resilience: Lessons from Kiribatidoctorswithoutborders.org
93. Water is life, how climate change Is threatening water security in Kiribatimsf.org.za
94. Erosionclimate.gov.ki
95. Inventory of Conflict and Environment (ICE), Kiribatimandalaprojects.com
96. Climate Change Impacts: Kiribati - Science Saucesciencesauceonline.com
97. Water security in a changing climate: Learnings from Kiribatidoctorswithoutborders.org
98. Kiribati: A Nation on the Frontline of Climate Change  - Systematic Observations Financing Facilityun-soff.org
99. Kiribati: Atolls and Marine Ecosystems - ScienceDirectsciencedirect.com
100. Animals in Kiribati - A-Z Animalsa-z-animals.com
101. PIPA — Big Oceanbigoceanmanagers.org
102. Final DRAFT K-NISSAP 3 MAY 2015 updated to 26 April 2016 1kiribati-data.sprep.org
103. Invasive Species Threaten Globally Important Seabirds in Kiribatisdg.iisd.org
104. KIRIBATI BIODIVERSITY AREA REPORT AUGUST 2013mfed.gov.ki
105. Flint Island (31302) Kiribati, Oceaniakeybiodiversityareas.org
106. Key Biodiversity Areaskeybiodiversityareas.org
107. Invasive Species Threaten Globally Important Seabirds in Kiribatisprep.org
108. Protection of Kiritimati Seabirds through Invasive Species Managementlibrary.sprep.org
109. Phoenix Islands Protected Areaalluringworld.com
110. Marine World Heritage - Phoenix Islands Protected Areavliz.be
111. Coral reefs of Kiribatien.wikipedia.org
112. Protected areas of Kiribatien.wikipedia.org
113. Status report for Kiribati's coral reefs Edward R. Lovell Taratau Kiratahorizon.documentation.ird.fr
114. The conservation and protection of seabirds in Kiritimati Island.panorama.solutions
115. Phoenix Islands Protected Area - UNESCO World Heritage Centrewhc.unesco.org
116. Birds, Birding Trips and Birdwatching Tours in Republic of Kiribati - Fat Birderfatbirder.com
117. Kiribati - Pacific Islands, Colonial Rule, Independencebritannica.com
118. The History of Kiribatikiribas.org
119. History of Kiribati: First People, British Rule and Independenceioa.factsanddetails.com
120. Micronesia - Ka'iwakīloumoku - Hawaiian Cultural Centerkaiwakiloumoku.ksbe.edu
121. History of Kiribatien.wikipedia.org
122. Lost Knowledge: Stick Chart Navigation - Make:makezine.com
123. Polynesian Stick Chartsthenonist.com
124. Test Your Sense of Direction with Star Maps and Stick Charts of Polynesian Wayfindersmessynessychic.com
125. Land Tenure Problems, Gilbert and Ellice Islandsrepository.si.edu
126. (PDF) Towards Colonial Protectorates: The Case of the Gilbert and Ellice Islandsacademia.edu
127. The History of Kiribati: Timeline.myvirtualworldtrip.com
128. Kiribati Historycountryreports.org
129. Japanese settlement in Kiribatien.wikipedia.org
130. Gilbert and Ellice Islandsen.wikipedia.org
131. (PDF) The Partition of the Gilbert and Ellice Islandsresearchgate.net
132. Visiting battle grounds: Tarawawm.awm.gov.au
133. Japanese occupation of the Gilbert Islandsen.wikipedia.org
134. Tarawa Invasion Casualitiesdpaa-mil.sites.crmforce.mil
135. The Battle of Tarawamarinesnz.com
136. Taniura Hideo at the Battle of Tarawawarfarehistorynetwork.com
137. Commemoration of the 80th Anniversary of the Battle of Tarawa - U.S. Embassy in Fiji, Kiribati, Naoero, and Tuvalufj.usembassy.gov
138. History of Kiribatien.wikipedia.org
139. Gilbert and Ellice Islandsbritannica.com
140. Battle of Tarawaen.wikipedia.org
141. States of Oceania - Kiribatihistoryfiles.co.uk
142. History of Kiribatibritannica.com
143. 1974 Ellice Islands self-determination referendumen.wikipedia.org
144. Tuvaluen.wikipedia.org
145. Constitution of Tuvaluen.wikipedia.org
146. Constitution of Kiribatien.wikipedia.org
147. Constitution of Kiribati, Kiribati, WIPO Lexwipo.int
148. Politics of Kiribatien.wikipedia.org
149. The Kiribati Independence Order 1979legislation.gov.uk
150. Constitution of Kiribati.fao.org
151. Kiribati 1979 (rev. 2018) Constitution - Constituteconstituteproject.org
152. Kiribati considers constitutional change to cement diplomatic recognition of China - ABC Newsabc.net.au
153. Independence For Kiribati - Hansard - UK Parliamenthansard.parliament.uk
154. Kiribati Members of the Maneaba ni Maungatabuopensanctions.org
155. KIRIBATI - General Elections - Regional Programme Australia and the Pacific - Konrad-Adenauer-Stiftungkas.de
156. Elections in Kiribatien.wikipedia.org
157. KIRIBATI Commonwealth Parliamentary Associationcpahq.org
158. 2024 Kiribati parliamentary electionen.wikipedia.org
159. Kiribatien.wikipedia.org
160. Judiciary of Kiribatien.wikipedia.org
161. Kiribati Court of Appealen.wikipedia.org
162. Kiribati's justice system under the spotlight following alleged political interferencenit.com.au
163. IPU PARLINE database: KIRIBATI (Maneaba Ni Maungatabu), ELECTIONS IN 2011archive.ipu.org
164. House of Assembly (Kiribati)en.wikipedia.org
165. Kiribati, Nauru and Tonga Admitted to United Nations Membershipmedia.un.org
166. The New Pacific Diplomacypress-files.anu.edu.au
167. Kiribati Foreign Relationsglobalsecurity.org
168. Pacific Islands Forumdppa.un.org
169. Foreign relations of Kiribatien.wikipedia.org
170. Kiribati — Foreign Policy & UN Votingmodeldiplomat.com
171. Kiribati Breaks Ties with Taiwan, Raising Fears That Other Diplomatic Allies Will Switch to Recognizing Chinanewbloommag.net
172. Taipei down to 15 allies as Kiribati announces switch of diplomatic ties to Beijingscmp.com
173. Island nation of Kiribati cuts ties with Taiwan, switches to Chinasbs.com.au
174. Taiwan and Kiribati sever ties after China switch - Asia Timesasiatimes.com
175. Written statement of the Republic of Kiribatiicj-web.leman.un-icc.cloud
176. Sea-Level Rise, Human Rights, and State Responsibility: Advisory Opinions in an Interdependent International Legal Orderdoi.org
177. Implications of sea-level rise on human rights - Amnesty Internationalamnesty.org
178. Rejecting Reality: Kiribati’s Shifting Climate Change Policiessites.utexas.edu
179. Between Migration and Resilience: Kiribati’s Strategic Dilemmaclimatalk.org
180. South Tarawaen.wikipedia.org
181. Tarawaen.wikipedia.org
182. Aroraeen.wikipedia.org
183. South Tarawa, Kiribatiebsco.com
184. Outer Islands Transport Infrastructure Investment Project (RRP KIR 53043)adb.org
185. CORVI Risk Assessment: Tarawa, Kiribati • Stimson Centerstimson.org
186. Labor Marketnso.gov.ki
187. [Working Draft] Joined ILO in 2000 Kiribati: Country Factsheet [Working Draft]ilo.org
188. Kiribati People 2024, CIA World Factbooktheodora.com
189. Kiribati - Population and Demography Country Profileourworldindata.org
190. FINAL APPROVED 20/01/2016 Kiribati Education Improvement Program (KEIP)dfat.gov.au
191. Kiribatieducation-profiles.org
192. Education in Kiribatien.wikipedia.org
193. Education in Kiribatiglobalpartnership.org
194. Education in Kiribati: Access for Older Students - The Borgen Projectborgenproject.org
195. Kiribati - Virtual Education Wikiopeneducation.wiki
196. Religion in Kiribatien.wikipedia.org
197. 2022 Report on International Religious Freedom: Kiribatistate.gov
198. 2020 Report on International Religious Freedom: Kiribatistate.gov
199. Catholic Church in Kiribatien.wikipedia.org
200. Kiribati Uniting Churchen.wikipedia.org
201. Gilbertese languageen.wikipedia.org
202. Kiribati Languages • FamilySearchfamilysearch.org
203. Kiribati's Languages - GraphicMaps.comgraphicmaps.com
204. What Languages Are Spoken In Kiribati?worldatlas.com
205. Education in Kiribati - Goals For Good Foundationgoals-4-good.org
206. Kiribati Culture & Way of Lifekiribatitourism.gov.ki
207. Maneabaen.wikipedia.org
208. MUSIC OF KIRIBATImacropsychic.substack.com
209. The Atoll Mindset: 10 Quirks of Kiribati Society That Reveal a Unique Worldviewvocal.media
210. Legislative Assemblyparliament.gov.ki
211. Culture of Kiribatien.wikipedia.org
212. Dance in Kiribatien.wikipedia.org
213. Culture & Island Explorekiribatitourism.gov.ki
214. Music of Kiribatien.wikipedia.org
215. The Music of Kiribati: Songs that Tell Storiesfarandawayadventures.com
216. Kiribati Heritage: An Atoll Nation Facing the Rising Seaconfinity.com
217. Kiribati History & Heritage 2025: Museums, Architecture & Historical Sitesatlas-guide.com
218. 1 Capacity Building Workshop on the Implementation of the UNESCOich.unesco.org
219. Islands and Tradition: Clothing, Dances, and Life in Kiribatien.postposmo.com
220. Te Umanibongen.wikipedia.org
221. House of Assembly (Kiribati)en.wikipedia.org
222. Dancing in Kiribatimyvirtualworldtrip.com
223. Fish for the future: Fisheries developmentdigitalarchive.worldfishcenter.org
224. Kiribati - Economyglobalsecurity.org
225. 2018-2022 Fishing License Revenuemfed.gov.ki
226. 2015 kiribati unsdpolicy.desa.un.org
227. Kiribatigfmd.org
228. www.fao.orgfao.org
229. FISHERY AND AQUACULTURE COUNTRY PROFILE Food and Agriculture Organization offao.org
230. © 2024International Monetary Fund IMF Country Report No. 24/104 KIRIBATIimf.org
231. Kiribati: Selected Issues in: IMF Staff Country Reports Volume 2024 Issue 104 (2024)elibrary.imf.org
232. High-Level Summary Technical Assistance Reports Volume 2024 Issue 042: Kiribati: Agricultural Subsidies for Copra: Improving Efficiency and Equity and Balancing Trade-offs (2024)elibrary.imf.org
233. Kiribati spends one dollar in three on households, minister writes - Solomon Times Onlinesolomontimes.com
234. Navigating the tides: how fiscal discipline sustains social protection in Kiribati - Devpolicy Blog from the Development Policy Centredevpolicy.org
235. 22,350 research outputs foundcore.ac.uk
236. Working overseas: Seafarers’ remittances and their distribution in Kiribati - Borovnik - 2006 - Asia Pacific Viewpoint - Wiley Online Libraryonlinelibrary.wiley.com
237. 5 Remittances and Migration in: Pacific Island Economieselibrary.imf.org
238. Save Kiribati - Economysavekiribati.com
239. Economy of Kiribatien.wikipedia.org
240. KIRIBATI STAFF REPORT FOR THE 2017 ARTICLE IV CONSULTATION—imf.org
241. Kiribati Government 2020 Recurrent Budgetpresident.gov.ki
242. KIRIBATI 4 INTERNATIONAL MONETARY FUNDelibrary.imf.org
243. Kiribati’s RERF Hits Historic $1.67 Billion Milestonemfed.gov.ki
244. © 2025 International Monetary Fund IMF Country Report No. 25/172 KIRIBATIimf.org
245. IMF Staff Completes 2026 Article IV Consultation to Kiribatiimf.org
246. IMF Staff Completes 2025 Article IV Consultation to Kiribatiimf.org
247. Kiribati: 2024 Article IV Consultation-Press Release; Staff Report; and Statement by the Executive Director for Kiribati in: IMF Staff Country Reports Volume 2024 Issue 103 (2024)elibrary.imf.org
248. Kiribati: 2026 Article IV Consultation-Press Release; Staff Report; and Statement by the Executive Director for Kiribati in: IMF Staff Country Reports Volume 2026 Issue 099 (2026)elibrary.imf.org
249. Kiribati: Staff Report for the 2024 Article IV Consultation—Debt Sustainability Analysis in: IMF Staff Country Reports Volume 2024 Issue 103 (2024)elibrary.imf.org
250. SREP Investment Plan for Kiribaticif.org
251. Project Number: 49450-021 November 2020adb.org
252. Kiribati Integrated Energy Roadmap: 2017–2025 July 2017irena.org
253. Kiribati—Assessment Letter for the Asian Development Bank October 25, 2022adb.org
254. IMF Executive Board Concludes 2026 Article IV Consultation with Kiribatiimf.org
255. Kiribati: Staff Report for the 2023 Article IV Consultation—Debt Sustainability Analysis in: IMF Staff Country Reports Volume 2023 Issue 329 (2023)elibrary.imf.org
256. Export Previewlca.logcluster.org
257. Getting Around - Kiribati for Travellersvisitkiribati.travel
258. Find Freight, Shipping and Logistics expertise in Kiribaticommonwealthofnations.org
259. Transport in Kiribatien.wikipedia.org
260. Cargo Servicesairkiribati.com.ki
261. Save Kiribati - Transportationsavekiribati.com
262. Save Kiribati - Getting Around Kiribatisavekiribati.com
263. Kiribati Grid Connected Solar Photovoltaic Projectdocuments1.worldbank.org
264. Kiribati's dependency on imported dieselebsco.com
265. Kiribati’s Over-Reliance on Fuel to End With World Bank Projectworldbank.org
266. Find Electricity and Power expertise in Kiribaticommonwealthofnations.org
267. Ground Breaks On Largest Solar PV Plant In Kiribatitaiyangnews.info
268. Kiribati Energy Storage Photovoltaic - SolarHome Systemsfenix-info.pl
269. Kiribatietcluster.org
270. Arrival of Submarine Cable a Milestone for High-Speed Broadband in Kiribatiadb.org
271. Improving digital connectivity in the Federated States of Micronesia, Kiribati and Nauru via submarine cableaiffp.gov.au
272. NEC completes construction of approximately 2,250 km EMCS submarine cable linking Pacific island nationsnec.com
273. 3.4 Kiribati Telecommunicationslca.logcluster.org
274. New era of connectivity as East Micronesia Cable lands in Kiribati - Australia Pacific Islands Business Councilapibc.org.au
275. NEC completes EMCS cable linking FSM, Kiribati and Nauru - Developing Telecomsdevelopingtelecoms.com
276. New undersea internet cable for Nauru, Kiribati and the Federated States of Micronesia will be funded by Australia, the US and Japan - ABC Newsabc.net.au
277. Ministry of Health and Medical Services Nawerewere, Tarawa, Kiribatiextranet.who.int
278. Save Kiribati - Healthsavekiribati.com
279. Health Service Delivery Profile Kiribati 2012mfed.gov.ki
280. Strengthening health emergency response capacity in Kiribati: establishing the Kiribati Medical Assistance Team (KIRIMAT)ncbi.nlm.nih.gov
281. Health workers on island nation of Kiribati face extraordinary challenges, including climate changedoctorswithoutborders.org
282. Kiribati: Remote island nation faces a triple threat to healthdoctorswithoutborders.org
283. Tuberculosis and diabetes mellitus in the Republic of Kiribati: a case–control study - Viney - 2015 - Tropical Medicine & International Health - Wiley Online Libraryonlinelibrary.wiley.com
284. Prevalence and spatio-demographic variability of nutrition-related health issues in Kiribatinature.com
285. Diabetes Statistics for Kiribatidiabetesatlas.org
286. Global Nutrition Reportglobalnutritionreport.org
287. Kiribati: Dedicated health professionals improve caremsf.org.au
288. Kiribati Annual Health Bulletin 2019 Kiribati Annual Health Bulletin 2019psro.dataforall.org
289. Kiribati: How dedicated women support healthcare on the islandsmsf.org.au
290. 1 >>> WORLD BANK GROUP KIRIBATI JOINT WORLD BANK -IMF DEBT SUSTAINABILITYdocuments1.worldbank.org
291. INTERNATIONAL DEVELOPMENT ASSOCIATION INTERNATIONAL MONETARY FUND KIRIBATIdocuments1.worldbank.org
292. Kiribati confronts climate upheaval by preparing for ‘migration with dignity’news.mongabay.com
293. Kiribati National Labour Migration Policymigrationnetwork.un.org
294. Rising seas & relocation: Climate struggles of Small Island Nationsvisionofhumanity.org
295. The migraine of migration: the tiny island-nation of Kiribati struggles for survivalcligs.vt.edu
296. Escaping a Rising Tide: Sea Level Rise and Migration in Kiribati - Wyett - 2014 - Asia & the Pacific Policy Studies - Wiley Online Libraryonlinelibrary.wiley.com
297. Limits in the Seas No. 146 Republic of Kiribatistate.gov
298. Reconsidering Sovereignty Amid the Climate Crisiscarnegieendowment.org
299. Kiribati Revenue Equalisation Reserve Fund (RERF) - LP Al...pipelineroad.com
300. Kiribati - Pacific Maritime Boundaries Dashboard - Pacific Data Hubpacificdata.org