{
"id": "sweden",
"title": "Sweden",
"lang": "en",
"source_lang": "en",
"summary": "Sweden is a Nordic country on the eastern Scandinavian Peninsula, known for its long north–south extent, forests, lakes, and archipelagos.",
"category": "geography",
"subcategory": "",
"type": "place",
"aliases": [
"Kingdom of Sweden",
"Sverige"
],
"generated_at": "2026-10-08",
"model": "pro/claude-haiku-5-5",
"url": "https://aiwiki.page/en/sweden/",
"translations": {
"zh-Hans": {
"url": "https://aiwiki.page/zh/sweden/",
"json": "https://aiwiki.page/zh/sweden.json"
}
},
"sections": [
{
"heading": "",
"text": "Sweden (Swedish: Sverige) is a country in Northern Europe that occupies the eastern and larger part of the Scandinavian Peninsula, within the wider Fennoscandian region. It covers roughly 450,000 square kilometres, including substantial inland water, and is home to about 10.6 million people, most of whom live in the south. Sweden shares land borders with Norway to the west and north and with Finland to the northeast, and it is linked to Denmark across the Øresund strait. Its coastline faces the Baltic Sea, the Gulf of Bothnia, the Kattegat and the Skagerrak.\n\nSweden's geography matters for understanding nearly every other aspect of the country. It stretches from temperate farmland in the south to subarctic and Arctic conditions in the north, so a single national territory contains very different climates, ecosystems and ways of life. Glaciated bedrock, mountains along the Norwegian border, and the many lakes and forests of the interior have shaped where people settle, how goods and people move, and which resources the economy depends on. The coast and its archipelagos connect the country to the rest of Europe through the Baltic and North Sea routes.\n\nThis entry first describes Sweden's location, borders and extremes, then its landforms and geology, its coast, islands and waters, and its climate. It then covers vegetation and land use, population distribution and the urban system, and administrative divisions. It closes with natural resources, protected areas, and the environmental changes and pressures that the country currently faces."
},
{
"heading": "Location, borders and extremes",
"text": "Sweden occupies the eastern and larger part of the Scandinavian Peninsula, which with Norway, Finland and the Kola Peninsula forms the Fennoscandian landmass. Its maximum north–south extent is about 1,574 km, while its greatest east–west breadth is about 499 km. Sweden is the largest of the Scandinavian countries, with about 15% of its total area situated north of the Arctic Circle.\n\nMeasured figures for the land borders vary between sources. The Swedish-language statistics cited by Norden give a total of 2,205 km, with 1,619 km shared with Norway and 586 km with Finland. IndexMundi, by contrast, lists Finland 545 km, Norway 1666 km. The gap is not an error in either source. IndexMundi notes that official lengths published by national statistical agencies are used when available, and because surveying methods may differ, country border lengths reported by contiguous countries may differ. The Finnish border is the main reason for the spread. Almost the entire border runs through water: along the Tornio River and its tributaries, and in the Gulf of Bothnia. A length based on river channels, banks or the thalweg will therefore differ from one based on a simplified line. The northern meeting point of the three countries lies at the Treriksröset cairn in Lake Koltajärvi, near Kilpisjärvi, which is also the northernmost point of Sweden.\n\nIn the south, Sweden has no land border, and its link with Denmark is maritime. The Øresund strait separates the Danish island of Zealand from the Swedish province of Skåne. The Øresund bridge and fixed link have connected two major metropolitan areas – Copenhagen, the capital of Denmark, and the Swedish city of Malmö. The crossing opened on 1 July 2000 and combines a cable-stayed bridge of about 7.8 km, an artificial island called Peberholm and a tunnel of about 4 km, which was chosen partly to keep ship and air traffic clear of each other. Skåne's southernmost tip, Smygehuk, Trelleborg in Scania, lies at roughly 55.34°N.\n\nThe extreme points are defined differently depending on whether islets and offshore features are included. For the mainland, one source places the easternmost point at Sundholmen, Haparanda in Norrbotten, at about 24.15°E, while another gives a longitude of 25°15′ E for the same mainland limit, so the exact figure is disputed. Offshore, the islet of Kataja in the Haparanda archipelago lies further east and is part of Sweden's border with Finland as well. The westernmost mainland point is Stensvik, Stromstad in Bohuslan, at about 11.11°E, whereas the westernmost point overall is the islet Stora Drammen off Kosteröarna.\n\nThe Arctic share also depends on definition. The astronomical line sits at 66°33′N, and roughly 15% of the national territory lies north of it. The Arctic Council instead treats the two northernmost counties as Sweden's Arctic territory, which represents about one-third of Sweden's territory, but is populated with just over half of a million inhabitants. Both figures are correct under their own criteria."
},
{
"heading": "Bedrock and landforms",
"text": "Most of Sweden rests on Precambrian crystalline rock. Geologists date this basement to a window that opens with the Earth's origin about 4,600 million years ago and closes at the start of the Cambrian, near 545 million years ago. Some time between the formation of the Earth about 4,600 million years ago and the start of the Cambrian period about 545 million years ago. The Swedish Geological Survey (SGU) divides the country's bedrock into three parts: this crystalline basement, a younger sedimentary cover, and the Caledonide mountain belt in the west. The solid rock geology of Sweden comprises three principal components, namely Proterozoic and locally Archean rocks, Phanerozoic sedimentary cover, and the early to mid-Paleozoic Caledonide orogen.\n\nThe basement forms the western part of the Fennoscandian Shield, which is the largest exposed area of Precambrian rocks in Europe. The shield has been consolidated over a very long time, and consists of old crystalline and metamorphic rocks. Gneiss and granite dominate the exposed rock, alongside granodiorite, sandstone and marble. In a few places in south-central Sweden the shield is capped by younger strata. Six such areas preserve early Paleozoic deposits, including roughly 200-metre-thick Cambrian quartz sandstone and Ordovician black shale, which lie unconformably on the older rock. Made up of 200 meter thick Cambrian shallow marine quartz arenite, as well as black shales from the Ordovician, and Silurian limestone, sandstone and shale.\n\nThe mineral wealth of the basement is concentrated in places such as Bergslagen in south-central Sweden. The district holds thousands of deposits, and iron oxide ores and zinc-lead-silver ores are the most numerous and the most historically important. The region hosts thousands of mineral deposits of various types, of which Fe oxide and Zn-Pb-Ag-(Cu-Au) deposits are the most abundant and historically most important. Mining there has continued for centuries, and the Garpenberg mine lies within the district. These rocks were also heavily reworked. During the Svecokarelian orogeny, roughly 1.89 to 1.75 billion years ago, the Bergslagen rocks were metamorphosed to amphibolite grade, meaning they were subjected to high temperature and pressure that recrystallized them. The district underwent amphibolite-grade metamorphism (with local areas of granulite and greenschist facies) during the Svecokarelian orogeny (1.89-1.75 Ga).\n\nMountains and the highest point\n\nThe western edge of the country is defined by the Scandinavian Mountains, which follow the Norwegian border. The Caledonides, the younger mountain belt that underlies them, built up about 500 to 400 million years ago. The highest summit in Sweden is Kebnekaise, a massif in Swedish Lapland. The Kebnekaise massif, which is part of the Scandinavian mountain range, has two main peaks. It lies about 150 kilometres (93 mi) north of the Arctic Circle. The massif's southern peak is glaciated, and it used to be the top of the country, but it has lost height. The glaciated southern peak used to be the highest at 2,120 metres (6,960 ft) above sea level, but has shrunk by 24 meters during the last 50 years, leaving the ice-free northern peak at 2,096.8 metres as the highest point. Measurement sources do not agree on the date of this change. Researchers at Tarfala first confirmed the north peak was higher in August 2018, while the Swedish Tourist Association describes the north peak as the highest point since 2019. The southern peak continued to lose height, and in 2021 it was measured at 2,094.6 metres, the lowest height since measurements began in the 1940s. On the wider scale, Norway holds the higher peaks: Galdhøpiggen in South Norway is the highest peak in mainland Northern Europe, at 2,469 metres.\n\nOutside the mountains, the terrain changes character. The south and east are mostly low plains and gently rolling hills, while the north is more rugged, with highland and mountain terrain that rises toward the west. Those lowlands carry most of the country's population and farmland, which is why the contrast in terrain matters for later sections.\n\nGlacial features and post-glacial uplift\n\nMost of the surface landforms owe their shape to the Quaternary ice sheets. The overburden is mainly formed by numerous periods of glaciation and deglaciation. The most common soil type is till, covering about 75 % of the landscape. Moraines are among the most common features. These ridges are moraines and provide evidence of former ice margins. Terminal moraines mark the furthest extent of an advance, while recessional moraines record a glacier that was retreating. Between Lake Vänern and Lake Vättern, a detailed LiDAR-based survey recognized fifteen landform types, including end moraines, drumlins, crag-and-tails and eskers. The area includes moraines associated with the Younger Dryas cold interval and drainage deposits of the Baltic Ice Lake.\n\nEskers are long, winding ridges of sand and gravel that were deposited by meltwater streams. A long, narrow, winding ridge composed of stratified sand and gravel deposited by a subglacial or englacial meltwater stream. The Swedish word ås, meaning ridge, is the origin of the synonym \"os\". Sweden is home to one of the longest eskers, Uppsalaasen, which stretches for about 250 kilometers and passes through the city of Uppsala. Erosion also left distinctive hollows. Broad trenches, depressions and rock basins occur in fracture zones between hill groups.\n\nOnce the ice melted, the land began to rise, a process known as post-glacial rebound or isostatic uplift. This lifted old shorelines out of the sea and left raised beaches across the coastal lowlands. Although the map is focused on glacial geomorphology, three units – shorelines, sand dunes and landslide scarps – are postglacial. The uplift also reshaped human geography. In Lake Mälaren, due to the post-glacial rebound, Södertälje canal and the mouth of Riddarfjärden bay had become so shallow by about the year 1200 that ships had to unload their cargoes near the entrances. The decline of Birka and the subsequent foundation of Stockholm at the choke point of Riddarfjärden were in part due to the post-glacial rebound changing the topography of the Mälaren basin."
},
{
"heading": "Coastline, islands and archipelagos",
"text": "Length of the coast and its sea basins\n\nThere is no single agreed figure for Sweden's coastline, because the answer depends on how closely the shore is traced. A territorial baseline that includes Gotland and Öland comes to about 2,862 km, while the physical shore is put at roughly 7,264 km, and tracing every small indentation could push the total toward 14,000 km Its moderately indented territorial coastline, bounded by the Skagerrak and Kattegat to the southwest and by the Baltic Sea and its northern arm, the Gulf of Bothnia, to the east, and including the islands of Gotland and Öland, totals 2 862 km in length. The shore itself measures 7 264 km, and if one were to include all the little indentations, it could be said to total 14 000 km in length.. Some popular travel sites give a much shorter figure of about 3,218 km, which shows how far the estimates diverge.\n\nThe coast belongs to three water bodies. The southwest faces the Skagerrak and Kattegat, the south and east face the Baltic Sea proper, and the northeast faces the Gulf of Bothnia, which is divided into the Bothnian Bay and the Bothnian Sea. The gulf is long and narrow: it runs about 725 km north to south but only 80 to 240 km east to west Covering an area of about 45,200 square miles (117,000 square km), the gulf extends for 450 miles (725 km) from north to south but only 50 to 150 miles (80 to 240 km) from east to west.\n\nIslands and the problem of definition\n\nSweden is often described as the country with the most islands, but the count depends on what is treated as an island. Official Swedish research has reported 221,831 islands, while a 2013 statistics report counted 267,570, of which fewer than 1,000 are inhabited A 2013 statistics report concluded that there are 267,570 islands in Sweden, though fewer than 1,000 of these are inhabited.. The gap reflects the threshold used. A widely used European definition, which requires a minimum area of one square kilometre, a distance of one kilometre from the shore, and more than 49 inhabitants, would reduce the count for Sweden to 24 If we go with the European definition of an island being a minimum of a square kilometre in size, must be one kilometre from the shore, not connected to the mainland, has more than 49 inhabitants, and does not contain a capital of the European Union (sorry Stockholm, guess you're out), then there are only 24 islands.. Lower thresholds also add a great many rocks: a list for the Bothnian Bay, which counts any land area above 20 square metres surrounded by water, includes 4,001 islands A list of islands of Bothnian Bay would include 4,001 islands if an island is defined as an area of land more than 20 square metres (220 sq ft) that is surrounded by water..\n\nArchipelagos and the largest islands\n\nThe archipelago around Stockholm is the largest in Sweden and the second largest in the Baltic, after the Archipelago Sea in Finland the largest archipelago in Sweden, and the second-largest archipelago in the Baltic Sea. Its total is usually given as slightly over 24,000 islands, islets and skerries, covering about 1,700 km², of which roughly 530 km² is land Stockholm Archipelago has been found to have slightly over 24,000 islands, islets and skerries and covers approximately 1,700 km² of which approximately 530 km² is land.. Its island population is concentrated in a relatively small number of settled islands, with many holiday homes among them.\n\nGotland is the largest island. Estimates range from about 2,994 km² to about 3,184 km², the higher figure including its smaller satellites. Its coastline is about 800 km long including Fårö Coastline: 800 km (500 mi) (including Fårö). Gotland is a province fully integrated into Sweden, without the autonomy enjoyed by some other island groups in Europe Gotland is a fully integrated part of Sweden with no particular autonomy, unlike several other offshore island groups in Europe.. Öland, further south on the east coast, is the second largest, at about 1,342 to 1,347 km². Värmdö, the largest island of the Stockholm archipelago, is third on the eastern coast at about 181 km² Värmdö is after Gotland and Öland the third largest island on the eastern coast of Sweden..\n\nBrackish water and its consequences\n\nMost of Sweden's coast lies in the Baltic, which is brackish, meaning its salt content is low. Salinity on the small west coast is about 20 parts per thousand, but the rest of the Swedish coast is far less salty Although the salinity on the small west coast of Sweden is about 20 ppt, the salinity off the remainder of the Swedish coast, as with other areas of the brackish Baltic basin, is low.. One estimate suggests that roughly 5,700 km of the 7,600 km coastline is brackish Ackefors (1986) considers that about 5 700 km of a 7 600-km coast is brackish..\n\nThe low salinity is most pronounced in the north. Many rivers drain into the Gulf of Bothnia, so its water is very fresh, and ice can persist for up to five months each winter Because it receives the water of so many rivers, including the Ångerman, Ume, Lule, Torne, Kemi, and Oulu, its salinity is extremely low, and, in consequence, ice cover is maintained for up to five months in the winter.. The Bothnian Bay itself is frozen for roughly 110 to 190 days a year Frozen: 110–190 days annually. Because the sea is fresh enough for many freshwater species to survive yet salty enough for some marine species to matter, the Baltic supports fewer species than a full-strength ocean, and this shapes both the marine ecosystem and the fishing and port activity of coastal towns such as Luleå, Härnösand, Sundsvall and Gävle, which are the main gulf ports on the Swedish side."
},
{
"heading": "Lakes, rivers and inland waters",
"text": "How many lakes\n\nSweden's inland waters are extensive for a country of its size, but any count depends on the size threshold. One list cites 22,600 lakes larger than 0.1 km² and over 97,500 lakes larger than 2 acres (8,100 m²). Other estimates put the total at from 96 000 to 100 000 in number, and the Uppsala University lake mapping project has reported figures that differ significantly from the assumptions previously made. Inland water covers roughly almost 9 percent of the territory, and with the 0.1 km² threshold Sweden ranks fifth among countries with most lakes in the world.\n\nThe three great lakes\n\nVänern is the largest. Its area is given as 5,519 km² in ranked lists and 5,650 km² in other sources, a gap that reflects different survey methods rather than a disagreement about the lake itself. Its average depth is 27 m, its maximum depth is 106 m, and its water volume is about 153 km³. The main inflow is the Klarälven, which enters Vänern near Karlstad with its source in Trøndelag in Norway. The lake drains westward through the Göta älv to the Kattegat, and the Göta älv is a major source of hydroelectric power.\n\nVättern, the second-largest lake, is a long, finger-shaped body of fresh water in south central Sweden. It is much deeper than its area suggests: it contains roughly half as much water as Vänern even though it covers about a third as much area, and its deepest point lies 128 metres below sea level. Its outflow is the Motala ström.\n\nMälaren, the third-largest, is 120 km (74.6 mi) from east to west and drains into the Baltic through its natural outlets Norrström and Söderström, which pass Stockholm's city centre, as well as an artificial canal. Its area is usually given as 1,090 km², though other sources use 1,140 km². Its many islands make it seem larger than it is, and it is the lake that brings fresh water close to Stockholm.\n\nLakes in the interior and the north\n\nBeyond the top three, the largest lakes include Hjälmaren, Storsjön and Torneträsk, with Hornavan being the deepest lake in the country, located in Norrland. Norrland's lakes are often long narrow high level lakes formed mostly by moraines, which dammed meltwater behind debris left by the ice. The north's lake country is therefore largely a product of glacial deposition, whereas the south's many small basins are often attributed to erosion. Alfred Nathorst argued that the great number of lakes in southern Sweden could be indebted to the creation of basins due to the stripping of an irregular mantle of weathered rock by glacier erosion. The sources I consulted do not establish a clear regional count showing most lakes lie in Norrland, so the claim that the north holds the largest number should be treated cautiously.\n\nRivers and hydropower\n\nNorrland, which covers about 60 percent of the country, is drained by long rivers. Its rivers rise in mountains exceeding 1 500 m in height and flow in a series of steps, crossed by parallel rivers in deeply cut valleys. The Lule river is typical: it flows southeast from the mountainous Sarek wilderness along the Norwegian border and reaches the Gulf of Bothnia at Luleå, covering about 460 km. Before dams and power stations, many of these rivers were used to transport timber down to the sawmills near the coast.\n\nThe steep gradients made Norrland central to Swedish hydropower. The hydropower production in Norrland stands for 80 % of national output. Among the rivers, the river Lule älv is the most important river in Sweden for the generation of hydro power. Its Harsprånget station, with an installed capacity of 811 MW, is the largest in the country. Development began early: Porjus was built in the early 1900s to supply electricity to the Malmbanan railway line, which was used to transport iron ore. Hydropower has been constrained by policy as well, and 42 watercourses are protected from expansion of hydropower.\n\nThe Göta Canal and other waterways\n\nThe Göta Canal was built in the 19th century to link the coast with the interior lakes. It runs from the west coast to Stockholm, and the lake forms a major link in the Göta Canal. Its route combines artificial cuts with the natural lakes Vänern and Vättern and navigable river sections. Improvements to the Trollhätte Canal allow seagoing craft entering from the Kattegat to serve such lake ports as Karlstad, Lidköping, Vänersborg, and several other inland towns. The canal shows how Sweden's lakes and rivers have shaped its transport network as much as its energy supply."
},
{
"heading": "Climate",
"text": "Sweden has no single climate. Its territory runs from about 55°N in Skåne to about 69°N in the north, and this range places the far south in a mild, maritime regime while the north has a subarctic one. In the far south, winters are usually weak, with only brief spells of snow and sub-zero temperatures, and autumn can pass almost directly into spring. Classification depends on the threshold used. Using the 0 °C isotherm, the coastal south counts as humid continental; using the –3 °C isotherm, it counts as oceanic. The central parts fall into the humid continental band, and the north falls into the subarctic class, which is a Köppen Dfc climate in most localities.\n\nLatitude is the main control, but the surrounding seas moderate it. Sweden is much warmer and drier than other places at similar latitudes, chiefly because the Gulf Stream and the prevailing westerlies deliver heat and moisture from the Atlantic. The Scandinavian Mountains along the Norwegian border intercept much of the wettest maritime air, so the western slopes receive more precipitation and the eastern interior becomes drier and more continental. The mountains also shape temperatures in a less obvious way: Östersund, in the north, has milder winters than most places at similar latitudes, because Atlantic air reaches it through passes in the range, whereas Hoting, farther inland and away from both the Atlantic and the Gulf of Bothnia, has colder winters for its latitude. The interior is also warmest in summer in the Mälaren Valley around Stockholm, which is shielded from Atlantic low-pressure systems by the surrounding land. Temperature gradients are steep: the difference between the southernmost and northernmost coastlines is about 2 °C in summer and 10 °C in winter, while in the northern interior the winter gap reaches about 15 °C.\n\nSeasonal extremes are most pronounced in the north. Stockholm's average daily high is about –1 °C in January and about 22 °C in July, with average lows near –5 °C in January. In Norrland, winters are long and sub-zero with considerable snow, while summers are short and mild, though they occasionally reach around 30 °C. North of the Arctic Circle, the sun stays below the horizon for part of the winter, producing polar night, and stays above it through part of the summer, producing the midnight sun. Svealand has winters just below zero with frequent snowfall, particularly in the northwest where most ski resorts are located, whereas Götaland has shorter, milder winters with little snow. Snow cover therefore lasts longest in the mountains and the north and becomes shorter and less reliable toward the south; the exact duration varies considerably from year to year.\n\nSea ice is a distinct climatic feature of the Baltic. The Baltic is brackish, shallow and nearly enclosed, which produces strong seasonal variation in ice extent, thickness and duration. In an average winter, about half of the Baltic's surface is ice-covered. Ice is most persistent in the northern basins, including the Bothnian Bay, where ice conditions are the most demanding for navigation. Because ice makes the sea hazardous for both passenger and cargo vessels, winter navigation there has depended on icebreaking since state-led icebreaking began in 1890, when the practice shifted from simply closing ports for the season to assisted winter navigation. Traffic in the Baltic is regulated through Finnish–Swedish ice-class rules, which set the minimum hull requirements for ships that receive icebreaker assistance. In one severe season, the worst ice cover since 1996 trapped about 50 cargo and passenger vessels between Sweden and Finland for several days, and they had to be freed by icebreakers. The 2025–2026 winter again put the Swedish fleet under strain: all available icebreakers were mobilised, and the narrow Kalmarsund was temporarily closed, forcing vessels to reroute around Öland with longer transit times and higher costs. The Swedish Maritime Administration has since commissioned a larger replacement vessel for delivery in the 2029–2030 icebreaking season, because the older icebreakers are nearing the end of their technical lives."
},
{
"heading": "Vegetation and land use",
"text": "Forest cover\n\nForest is the dominant land cover, but the exact share depends on the source and its date. A recent World Bank-based figure puts forest at 68.7 percent of the land area, forestry bodies describe it as nearly 70 percent, and older studies give figures closer to 60 percent. These gaps most likely reflect changing definitions of \"forest\" and different inventory methods, not a simple loss of woodland. Most of the cover is boreal forest (taiga), a belt of coniferous and birch-dominated woodland that covers the north and the central regions beyond the mountains. Forest cover is highest in the north and centre, where some areas exceed 80 percent, while the south is a mosaic of woodland and open farmland. In the late 1990s, the south-western county of Malmöhus (now part of Skåne) had only about 18 percent forest.\n\nForest ownership is unusually diverse. Roughly half of the forest land belongs to around 300,000 private family owners, about a quarter to companies, and the rest to the state, the Church of Sweden and other bodies. Production forestry relies mainly on clear-felling, with about 1 percent of productive forest land harvested each year and replanting required by law. Formal protection covers only a small part of the forest estate: a 2022 national count gave about 2.4 million hectares of formally protected forest land, and a further large area of unproductive forest is recorded separately, much of it overlapping protected areas.\n\nAgricultural land\n\nAgricultural land occupies just over 3 million hectares, about 7 percent of the national territory. Arable land makes up about 6 percent, roughly 2.5 million hectares in 2023, which is far below the global average of around 14 percent. Cropland is concentrated in the south-central and southern plains, where soils and a relatively long growing season allow cereal and oilseed production. Grain occupies about 1 million hectares, forage crops just over 1 million, and the remainder goes to rapeseed, potatoes, sugar beet, protein crops and fallow. Arable grassland, around 1.1 million hectares, is partly kept open largely for subsidy eligibility and is only lightly used.\n\nThe arable area has been shrinking for decades. Official FAO-based series show a fall from about 3.5 million hectares in 1961 to about 2.5 million in 2023, and the decline had continued for fourteen consecutive years by the latest figures. Rising yields mean that less land is needed to produce a given harvest, and farmland has also been lost to roads and urban development. Since 1970 about 400,000 hectares of arable land has been abandoned, and much of it has been overgrown by forest plantations.\n\nPeatlands, mires and wetlands\n\nPeatlands are most extensive in the north, although the figures vary with the definition used. One estimate of peatland area is 65,600 square kilometres, while mapping based on Quaternary deposits gives between about 62,000 and 69,000 square kilometres. A national count of peat-covered land with a deposit deeper than 30 centimetres gives about 6.4 million hectares. Mean peat depth is greater in the south, at about 2.3 metres in Götaland, than in Norrland, at about 1.5 metres, so the south has thicker peat on less total area. Mire types also differ by region. The south is dominated by raised bogs, which receive water only from precipitation, and by flat fens on the plains. The north has mosaics of bog and fen, and the far north has aapa mires with strings and flarks, the patterned surfaces typical of northern Fennoscandia. Large areas of northern mire are in fact forested wetlands, and willow scrub is common on flooded land near watercourses.\n\nDrainage has altered many of these wetlands. In the 1950s about 10 percent of the agricultural area was drained wetland, and some studies estimate that more than half of Sweden's natural peatlands have been drained for forestry, agriculture or peat extraction. Drainage of intact peatlands to improve timber production was ended in 1986. Today new drainage is banned in southern Sweden, while in most of the central and northern regions it remains legal after consultation, except in coastal areas. Restoration has focused on rewetting former peat extraction sites, and the Swedish government has designated Ramsar wetlands of international importance, several of them in the north.\n\nPasture and other land\n\nPermanent pasture is a very small share of the territory, around 464,000 hectares or about 1.1 percent of the land in 2022. Other land uses, including built-up areas, roads, barren ground and unproductive land, make up roughly a quarter of the total. Because the sources available do not provide a long national series for permanent pasture alone, the trend is best read through the broader pattern: open farmland has been abandoned and overgrown, arable area has contracted, and forest has expanded into former fields and meadows."
},
{
"heading": "Population distribution and urban system",
"text": "Sweden has about 10.6 million inhabitants and is the most populous of the Nordic countries. At 450,295 square kilometres and with a population of 10.6 million, Sweden is the largest and most populous Nordic country. The national average density of roughly 25 people per square kilometre is misleading. Part of the reason is that the total area includes large areas of lakes and other inland water; by one count, the total land area is 410,340 Km², so the per-hectare figure for land is somewhat higher. The larger problem is that the average blends very different regions. Settlement is dense in the south and centre and very thin in the north. Most people live in towns, but built-up land is a small share of the country: 88% of Swedes reside in urban areas, while Sweden's urban areas together cover 1.5% of its land area.\n\nThe contrast between regions is stark. North Sweden, a NUTS-1 statistical region covering the northern part of the country, had a population (2024) of 1,758,372 spread over about 310,000 km², which gives a density of under 6 people per square kilometre. South Sweden, by comparison, had over 1.5 million in 2024 on about 14,000 km², giving a density above 110 per square kilometre.\n\nPopulation is concentrated around three large city regions: Stockholm, Gothenburg and Malmö. The figures for each depend heavily on how the area is defined. The Stockholm urban area, a continuous built-up zone, extends into 11 municipalities in Stockholm County, and as of 31 December 2019, the population in the Stockholm urban area was 1,593,426 inhabitants. A broader metropolitan definition gives much larger numbers. A comparative table based on 2018 functional-area estimates lists Stockholm with 2,308,143 people in its metro area, Gothenburg with 1,021,831 and Malmö with 669,471. Estimates for Malmö's metropolitan area have since risen; one demographic database puts it at 784,412 [in 2025] – estimate, which shows how quickly figures change with method and date. The municipality of Malmö itself, Sweden's third-largest city, had a municipal population of 365,644 in 2024.\n\nThe Øresund region links Malmö and the Scanian coast with Copenhagen across the strait. Its total population is about 3.8 million, and 3.8 million, of whom 2.5 million live on the Danish side. The fixed link has been central to integration: the bridge was completed in 2000, and since then the Oresund bridge has allowed Danes and Swedes to cross the Oresund strait in increasing numbers. Cross-border commuting is significant but still limited. Official figures put the 19 000 cross-border commuters, around 90 % commute from Sweden to Denmark. Surveys suggest that many residents do not see commuting as an attractive option; only 17% of the respondents from the Swedish side said that they were likely to look for a job in Denmark.\n\nAway from these centres, many northern and rural municipalities have seen their populations stagnate or fall as younger residents move to the larger cities and the south. Settlement in the north is sparse, and services and jobs are concentrated in a few towns. The north is also the homeland of the Sámi, the Indigenous people of Sápmi, whose traditional territory extends across northern Sweden, Norway, Finland and the Kola Peninsula. Sámi communities in Sweden have their own representative body, the Sámi Parliament, and traditional livelihoods such as reindeer herding are closely tied to the northern landscape."
},
{
"heading": "Administrative divisions and regions",
"text": "Sweden's territory is described through three overlapping frameworks: three traditional \"lands,\" 21 counties, and 25 historical provinces, with 290 municipalities at the base of local government. Only the counties, regions and municipalities have a formal administrative role today. The lands and provinces survive mainly as geographic and cultural reference points.\n\nThe three traditional lands\n\nSweden is traditionally divided into three lands from north to south: Götaland, Svealand and Norrland. Although Norrland does not serve any administrative purposes, it continues to exist as a historical, cultural, and geographic region, and the same is true of the other two.\n\nNorrland is the northernmost, largest and least populated of the three, and covers 261,292 km². Its share of the national territory is reported inconsistently: one source gives about 58 percent, while another says about 60 percent. The sources do not state which area data or boundary definitions they use, so I cannot say which figure is more precise. Svealand, the historical core in south-central Sweden, covers 91,098 km². Götaland takes in the Småland highlands and the plains of Skåne at the southern tip. Its area is not given in the sources I found. By my own arithmetic, subtracting the two figures above from the national total gives roughly a fifth of the country. The national total itself varies between sources, from 447,425 km² to 449,964 km².\n\nCounties (län)\n\nSweden has 21 counties. The county level was first established in the 1634 Instrument of Government, when it replaced the older provinces as the unit of state administration. The present map is more recent. Skåne was formed in 1997 through the merger of two earlier counties, and Västra Götaland followed in 1998. Each county has a state county administrative board, and each also constitutes its own region. The regions are responsible for health care and public transport, and the former county councils were restructured and renamed in 2020. Gotland is unusual in that the island of Gotland is both a region and a municipality. County populations also differ widely, with Stockholm County holding more than 2.4 million residents while Gotland has about 61,000 residents.\n\nProvinces (landskap)\n\nSweden has 25 provinces, which are historical, geographical and cultural regions. They have no administrative function, but retain their own cultural identities, dialects and folklore. Several were administrative units until the county system replaced them. Provincial and county borders do not line up consistently. Småland, for example, is split mainly between Jönköping, Kronoberg and Kalmar counties. Residents often identify with their province rather than their county, and provincial names still appear in everyday life.\n\nThe provinces are grouped by land. Norrland contains nine, Svealand six, and Götaland ten, which together make 25. Some boundaries have shifted over time. Norrbotten was part of Västerbotten which extended all the way to Österbotten in today's Finland before 1809.\n\nMunicipalities (kommuner)\n\nThere are 290 municipalities, which are responsible for a large proportion of local services, including schools, emergency services and physical planning. Each municipal assembly is composed of members elected by direct universal suffrage for a four-year term, and it also levies taxes and adopts the municipal budget. The executive committee is appointed by the municipal assembly. Municipalities sit inside counties, and since 2004 their number has been 290, thus an average of 13.8 municipalities per county. The number was reduced sharply in the 1960s and 1970s, from 1006 to 848 between 1965 and 1969, and it fell to 278 three years after the unitary municipality was introduced. The current figure of 290 was reached later.\n\nWhy the counts differ\n\nThe counts vary because the systems measure different things. The 21 counties and 21 regions cover the same territory, so they should not be added together. Legally, Sweden has 310 local administrations, which include the 290 municipalities and the 21 regions. Sources also differ on when the municipal total reached 290. One says the figure has been unchanged since the municipal reform of 1974, but this conflicts with the 278 figure cited above for that year. Finally, the historical lands are not fixed. Older accounts describe four \"lands\", including Österland, which covered southern and central Finland from the 13th century to 1809. The modern three-land scheme is therefore a simplification of a longer history."
},
{
"heading": "Natural resources and economic geography",
"text": "Sweden's economic geography rests on three resource bases that are unevenly spread across the country: forest, which covers most of the south and centre, iron ore and other minerals concentrated in the far north, and running water in the northern and central river systems. Where these resources lie, together with the coast and the main population centres, largely explains where industry, towns and transport routes developed.\n\nForest is the most widespread resource. Forest land covers roughly 70 per cent of the country, and about three-quarters of it is actively managed, while the rest is protected, set aside or unproductive. Ownership is divided among private individuals, forest companies and the state, and large industrial owners hold a significant share. Sweden has under 1 per cent of the world's commercial forest, yet it is a major exporter of sawn timber, pulp and paper, and the forest industry accounts for roughly a tenth of goods exports. Sawmills and pulp and paper mills were historically built at river mouths and on the coast, where logs could be floated down and shipped out, and this pattern of industrial sites persists. Forest industry is therefore a key employer in rural regions, even though its output is spread thinly over the landscape.\n\nIron ore is the main mineral resource, and it is concentrated in Norrbotten county in the north. The state-owned company LKAB operates mines at Kiruna and Malmberget and is described as Europe's largest iron ore producer. The Kiruna ore body has supplied more than 950 million tonnes since mining began in 1898, but only about a third of the deposit has been extracted so far. The deepening of the mine has required the relocation of parts of the town and its rail infrastructure. Sweden also mines copper, zinc, lead, gold and silver, mainly through the company Boliden. In 2023 the country extracted just over 84 million tonnes of ore. Most of the iron ore is hauled by rail to the ice-free port of Narvik in Norway, with a smaller share sent to Luleå, from where it is shipped to Baltic customers or processed at steelworks in Luleå and Oxelösund. Mining thus underpins the economies of northern municipalities, though its long-term future is tied to decarbonising steel production; LKAB has postponed its shift to fossil-free sponge iron to the 2040s, and it has announced a temporary production cut at Kiruna for 2026.\n\nEnergy supply reflects the same geography. Hydropower provides around 40 per cent of electricity generation and is the largest source of renewable electricity. Its output depends on the height of the fall and the volume of water, which is why most capacity lies in the rivers flowing from the northwestern mountains to the Baltic, while most electricity is consumed in the south. Lake Vänern also serves as a reservoir for hydropower plants along the Göta River. Nuclear power is the other pillar of the system, and wind power has grown rapidly in recent years, while hydropower capacity has changed little since 2010. Because demand is expected to roughly double by 2045, the balance between north and south, and between regulated hydropower and intermittent wind and solar, has become a central planning question.\n\nTransport infrastructure is organised around a north–south corridor of rail and road that links the Øresund region and the southern cities with Stockholm and then northwards toward Luleå and the Norwegian border. The ore railway from Kiruna to Narvik, a route of about 170 kilometres within Sweden, is among the most heavily used freight lines in the country. Gothenburg and Malmö are the principal ports. Gothenburg is the largest port in Scandinavia and handles a large share of container and bulk trade, while Malmö connects Sweden with Denmark and the wider continent, which is why the region's transport links were strengthened by the Øresund crossing."
},
{
"heading": "Protected areas and World Heritage sites",
"text": "（见上文正文）"
},
{
"heading": "Environmental change and pressures",
"text": "Baltic Sea eutrophication and dead zones\n\nSweden's long coastline faces the Baltic, a brackish sea that is strongly layered. Less salty surface water lies above denser, saltier water, which makes it difficult for oxygen from the atmosphere to reach the deep layers. Deep basins are refreshed only briefly by saltwater inflows from the North Sea, and summer inflows have less potential to aerate the deep basins than winter inflows, because warmer water holds less oxygen. The result is an oxygen deficit that the sea's own structure makes hard to reverse. Roughly 20 percent of the Baltic's deep seafloor is anoxic, an area approximately 1.5 times the size of Denmark, and the Baltic Sea is home to seven of the world's 10 largest marine dead zones.\n\nThe main driver is nutrient enrichment. This is primarily due to fertilisers entering the Baltic Sea via rivers. Agriculture is the largest human-caused contributor, while sewage adds further nitrogen and phosphorus. Excess nutrients feed algae, which later die and sink, and microorganisms decompose the biomass, completely consuming the oxygen contained in the deep water. The problem is not new: the Baltic had periods of low oxygen in historical times, but it was not until the middle of the last century that anthropogenic eutrophication made the situation worse. Since the 1980s, inflows of oxygen-rich, high-salinity water through the Danish Straits have been reduced, which weakens the natural recovery mechanism.\n\nSeveral feedback loops keep the system in place. Oxygen-depleted water at the seafloor causes phosphate to dissolve and be released into the sediment and water column, which initiates a vicious cycle that promotes nitrogen-fixing cyanobacteria. Fishing pressure adds to this. Overfishing of Baltic cod has intensified the problem. Cod eat sprats, which eat microscopic zooplankton, which in turn eat algae. Fewer cod and more sprats mean more algae and less oxygen. Climate change is expected to make matters worse, since eutrophication and expansion of hypoxic areas will likely exacerbate in a warmer future climate. The effects are also economic: in 2005, on Öland itself, it was estimated that algal blooms resulted in losses of approximately €11 million for the tourism and fishing sectors.\n\nResponses include EU coordination, since the Baltic Sea has become the first \"macro-region\" targeted by the EU to combat pollution, dead zones and overfishing. Sweden has also tested engineered re-oxygenation: scientists in Sweden are testing an idea to pump oxygen into the Baltic Sea in an attempt to revive its dying ecosystem. Not all scientists, however, are convinced of the success of this Baltic deep-water oxygenation project. Cutting nutrient inputs remains the central approach, yet the sea's response is slow: dead zones, areas with less than 20 µmol O₂ per liter, have become larger and persist longer.\n\nForests and biodiversity loss\n\nForestry is the most documented pressure on Swedish land ecosystems. The sixth Swedish Red List, published on 24 March 2026, uses the International Union for Conservation of Nature (IUCN) Red List categories and criteria, and it was compiled by more than 100 species experts across the country. Of 24,829 species assessed, 6,156 are now red-listed and 2,910 are classified as directly threatened. This represents the fourth consecutive assessment in which the proportion of threatened species has risen. Birds and mammals are among the worst affected groups: 45 percent of assessed bird species, 36 percent of mammals, 32 percent of fish and 22 percent of butterflies are now red-listed. Some losses are stark. Two owl species, the barn owl and the snowy owl, are now classified as Nationally Extinct in Sweden.\n\nForest-dwelling species account for a large share of the list. About 2,000 forest-living species are red listed, and lack of continuity forests, meaning forests that have never been clear-cut, is one of the main reasons forest-dwelling species are listed. Of 2,050 species living mainly in forests, 1,375 are strongly negatively affected by felling according to reported assessment. The forest industry disputes the weight of logging in extinctions: since the 1950s, no species has disappeared from Sweden solely as a result of forestry, and the Red List says harvesting \"may have been a contributory factor\" in five species' disappearance, among many other causes. Non-forestry pathogens also play a role. For the first time, two widespread tree species, ash and elm, met the criteria for being threatened, because of ash dieback and Dutch elm disease.\n\nClimate change effects on the north\n\nProjections for Sweden were laid out in a 2007 government report, and their figures predate later assessments. They anticipated that in summer-time the climate will be warmer and drier, particularly in southern Sweden. Snow regimes would also change: warmer winters will result in less remaining snow cover, which will lead to a smaller spring flood. In the mountains, the mountains will largely turn to scrub, and the reindeer-herding industry and mountain tourism may be affected. The growing season is expected to lengthen, with areas of bare mountain expected to decrease in extent. The same report expected that a number of vector-borne infections will spread north.\n\nSea level rise is expected to be modest but persistent. Sea levels are expected to rise by 0.2 to 0.6 metres globally over the next hundred years, then continue to rise for many hundreds of years, and no melting of the ice caps in Greenland and Antarctica is included in the calculations. Sea levels are expected to rise by up to 0.2 metres in seas adjoining Sweden. Ice on lakes and rivers is already responding. A study using records reaching back to the 18th century found that increasing air temperatures reduce the duration of ice cover on lakes and rivers, which affects water quality, ecology and recreational use. Species are also sensitive to winter conditions. Research on Svalbard found that deeper snow hardly affected microarthropods in 2015, but decreased their densities after a milder winter in 2016. A Swedish peat-bog experiment reported that responses of oribatid mites to warming are positive in summer but negative in winter. Shifting climate zones are a broader concern, as a temperature rise may lead to a shift in vegetation zones and the extinction of certain species.\n\nPolicy responses and their evidence\n\nForest policy is among the best-evaluated responses. Evaluations have concluded that Sweden is not on track to meet its own national 2020 environmental goals for sustainable forests. Some measures have been adopted: the integration of conservation considerations within production forest, such as green-tree retention, has also increased. Whether these measures can offset the continued loss of old-growth habitat is contested, and biodiversity outcomes depend on how the old-growth forest and habitat networks are managed. Measures in energy and land-use policy, including the transition to renewable energy and agricultural nutrient management, are treated in the relevant sections of this entry."
}
],
"links": [
"habitat",
"renewable-energy"
],
"sources": [
{
"title": "Location, size, and extent - Sweden - located, area",
"url": "https://www.nationsencyclopedia.com/Europe/Sweden-LOCATION-SIZE-AND-EXTENT.html"
},
{
"title": "Facts about Sweden",
"url": "https://www.norden.org/en/information/facts-about-sweden"
},
{
"title": "Sweden Land boundaries - Geography",
"url": "https://www.indexmundi.com/sweden/land_boundaries.html"
},
{
"title": "Finland",
"url": "https://barrysborderpoints.com/country-visits/finland/"
},
{
"title": "Oresund Bridge: Connecting Sweden and Denmark",
"url": "https://www.ice.org.uk/what-is-civil-engineering/infrastructure-projects/oresund-bridge"
},
{
"title": "Sweden Locator Map - Interactive Map of Sweden",
"url": "https://www.map-of-sweden.com/sweden.htm"
},
{
"title": "Where is Sweden in the World?",
"url": "https://worldpopulationreview.com/countries/sweden/location"
},
{
"title": "Sweden",
"url": "https://arctic-council.org/about/states/sweden/"
},
{
"title": "Geography of Sweden - Confidus Solutions",
"url": "https://www.confiduss.com/en/jurisdictions/sweden/geography/"
},
{
"title": "The Most Extreme Points of Sweden",
"url": "https://www.worldatlas.com/articles/the-most-extreme-points-of-sweden.html"
},
{
"title": "Øresund Bridge: Engineering, Geography & History — Complete Guide",
"url": "https://geographyworlds.com/blog/oresund-bridge/"
},
{
"title": "The bedrock of Sweden",
"url": "https://www.sgu.se/en/geology-of-sweden/rocks/the-bedrock-of-sweden/"
},
{
"title": "Chapter 1 Introduction to the lithotectonic framework of Sweden and organization of this Memoir",
"url": "https://www.lyellcollection.org/doi/full/10.1144/M50-2019-21"
},
{
"title": "(PDF) Tectonic and metallogenic evolution of the Fennoscandian Shield: Key questions with emphasis on Finland",
"url": "https://www.researchgate.net/publication/262325318_Tectonic_and_metallogenic_evolution_of_the_Fennoscandian_Shield_Key_questions_with_emphasis_on_Finland"
},
{
"title": "Geology of Sweden",
"url": "https://www.sgu.se/en/geology-of-sweden/"
},
{
"title": "Geology of Sweden",
"url": "https://en.wikipedia.org/wiki/Geology_of_Sweden"
},
{
"title": "Synthesis of bedrock geology in the Bergslagen region, Fennoscandian Shield, south-central Sweden",
"url": "https://www.researchgate.net/publication/271988073_Synthesis_of_bedrock_geology_in_the_Bergslagen_region_Fennoscandian_Shield_south-central_Sweden"
},
{
"title": "Kebnekaise",
"url": "https://en.wikipedia.org/wiki/Kebnekaise"
},
{
"title": "Sweden’s Highest Mountain Shrinks by Two Metres in a Year As Glacier Melts",
"url": "https://mountainresearchinitiative.org/news/sweden-s-highest-mountain-shrinks-by-two-metres-in-a-year-as-glacier-melts/"
},
{
"title": "Scandinavian Mountains",
"url": "https://en.wikipedia.org/wiki/Scandinavian_Mountains"
},
{
"title": "Description of units in the geomorphic database of Sweden",
"url": "http://resource.sgu.se/produkter/sgurapp/s1304-rapport.pdf"
},
{
"title": "Full article: Glacial geomorphology between Lake Vänern and Lake Vättern, southern Sweden",
"url": "https://www.tandfonline.com/doi/full/10.1080/17445647.2020.1820386"
},
{
"title": "Esker",
"url": "https://www.britannica.com/science/esker"
},
{
"title": "Mountain And Glacial Landforms: What Is An Esker?",
"url": "https://www.worldatlas.com/articles/mountain-and-glacial-landforms-what-is-an-esker.html"
},
{
"title": "Full article: Glacial ripping: geomorphological evidence from Sweden for a new process of glacial erosion",
"url": "https://www.tandfonline.com/doi/full/10.1080/04353676.2020.1774244"
},
{
"title": "M%C3%A4laren",
"url": "https://en.wikipedia.org/wiki/M%C3%A4laren"
},
{
"title": "Climbing Kebnekaise",
"url": "https://www.swedishtouristassociation.com/guides/climbing-kebnekaise/"
},
{
"title": "Kebnekaise : Climbing, Hiking & Mountaineering : SummitPost",
"url": "https://www.summitpost.org/kebnekaise/151165"
},
{
"title": "Esker",
"url": "https://en.wikipedia.org/wiki/Esker"
},
{
"title": "Inland fisheries of Europe.",
"url": "https://www.fao.org/4/t0798e/t0798e13.htm"
},
{
"title": "Baltic Sea",
"url": "https://en.wikipedia.org/wiki/Baltic_Sea"
},
{
"title": "Gulf of Bothnia",
"url": "https://www.britannica.com/place/Gulf-of-Bothnia"
},
{
"title": "Why Does Sweden Have So Many Islands? (See the Amazing Total)",
"url": "https://scandinaviafacts.com/why-does-sweden-have-so-many-islands-see-the-amazing-total/"
},
{
"title": "List of islands of Sweden",
"url": "https://en.wikipedia.org/wiki/List_of_islands_of_Sweden"
},
{
"title": "Sweden has the most islands in the world, so which ones make for the perfect escape?",
"url": "https://www.messynessychic.com/2023/04/13/sweden-has-the-most-islands-in-the-world-so-which-ones-make-for-the-perfect-escape/"
},
{
"title": "List of islands of Bothnian Bay",
"url": "https://en.wikipedia.org/wiki/List_of_islands_of_Bothnian_Bay"
},
{
"title": "Stockholm Archipelago",
"url": "https://en.wikipedia.org/wiki/Stockholm_Archipelago"
},
{
"title": "Gotland",
"url": "https://en.wikipedia.org/wiki/Gotland"
},
{
"title": "V%C3%A4rmd%C3%B6 (island)",
"url": "https://en.wikipedia.org/wiki/V%C3%A4rmd%C3%B6_(island)"
},
{
"title": "Bothnian Bay",
"url": "https://en.wikipedia.org/wiki/Bothnian_Bay"
},
{
"title": "Sweden Maps & Facts - World Atlas",
"url": "https://www.worldatlas.com/maps/sweden"
},
{
"title": "The Largest Islands of Sweden",
"url": "https://www.worldatlas.com/articles/the-largest-islands-of-sweden.html"
},
{
"title": "List of lakes of Sweden",
"url": "https://en.wikipedia.org/wiki/List_of_lakes_of_Sweden"
},
{
"title": "The world’s lakes have finally been counted",
"url": "https://www.uu.se/en/news/2014/2014-09-03-the-worlds-lakes-have-finally-been-counted"
},
{
"title": "V%C3%A4nern",
"url": "https://en.wikipedia.org/wiki/V%C3%A4nern"
},
{
"title": "Lake Väner",
"url": "https://www.britannica.com/place/Lake-Vaner"
},
{
"title": "V%C3%A4ttern",
"url": "https://en.wikipedia.org/wiki/V%C3%A4ttern"
},
{
"title": "Norrland",
"url": "https://en.wikipedia.org/wiki/Norrland"
},
{
"title": "Sweden's biggest hydroelectric plant going strong after 56 years",
"url": "https://www.reliableplant.com/Read/18560/sweden's-biggest-hydroelectric-plant-going-strong-after-56-years"
},
{
"title": "Norrland",
"url": "https://www.britannica.com/place/Norrland"
},
{
"title": "Hydropower in Sweden",
"url": "https://www.diva-portal.org/smash/get/diva2:800244/FULLTEXT01.pdf"
},
{
"title": "Porjus - Vattenfall's power plants",
"url": "https://powerplants.vattenfall.com/en/porjus/"
},
{
"title": "Harspr%C3%A5nget hydroelectric power station",
"url": "https://en.wikipedia.org/wiki/Harspr%C3%A5nget_hydroelectric_power_station"
},
{
"title": "The Largest Lakes in Sweden",
"url": "https://www.worldatlas.com/articles/the-largest-lakes-in-sweden.html"
},
{
"title": "Top 8 lake vacations in Sweden",
"url": "https://visitsweden.com/what-to-do/nature-outdoors/top-lake-vacations/"
},
{
"title": "Geography of Sweden",
"url": "https://en.wikipedia.org/wiki/Geography_of_Sweden"
},
{
"title": "Sweden's largest lake - Nordstjernan",
"url": "https://nordstjernan.com/news/sweden/5508"
},
{
"title": "Why Does Sweden Have So Many Lakes?",
"url": "https://scandinaviafacts.com/why-does-sweden-have-so-many-lakes/"
},
{
"title": "Climate of Sweden",
"url": "https://en.wikipedia.org/wiki/Climate_of_Sweden"
},
{
"title": "A Closer Look at the Weather in Sweden",
"url": "https://www.remitly.com/blog/travel/weather-in-sweden/"
},
{
"title": "Subarctic climate",
"url": "https://en.wikipedia.org/wiki/Subarctic_climate"
},
{
"title": "Weather",
"url": "https://www.encountertravel.com.au/solo-travel/europe/scandinavia-explorer-solo-travel-tour/more-info/weather/"
},
{
"title": "%C3%96stersund",
"url": "https://en.wikipedia.org/wiki/%C3%96stersund"
},
{
"title": "Hoting",
"url": "https://en.wikipedia.org/wiki/Hoting"
},
{
"title": "Sweden Geography and Climate",
"url": "https://www.workingabroad.com/travel/sweden-geography-and-climate/"
},
{
"title": "Climate of Sweden: Weather, Seasons & Best Time to Visit (2026)",
"url": "https://geographyworlds.com/blog/climate-of-sweden/"
},
{
"title": "The climate of Sweden and the best time to visit",
"url": "https://weatherandclimate.co.uk/sweden/"
},
{
"title": "Maritime operations in ice-covered waters: A 25-year data-driven study of baltic sea ice conditions and icebreaker-ship operations - ScienceDirect",
"url": "https://www.sciencedirect.com/science/article/pii/S0925753526001268"
},
{
"title": "ESA - Earth from Space: Baltic sea ice",
"url": "https://www.esa.int/Applications/Observing_the_Earth/Earth_from_Space_Baltic_sea_ice"
},
{
"title": "Russia Sends Nuclear Icebreaker From Arctic to Baltic Sea as Severe Ice Chokes Shipping",
"url": "https://gcaptain.com/russia-sends-nuclear-icebreaker-from-arctic-to-baltic-sea-as-severe-ice-chokes-shipping/"
},
{
"title": "Sweden orders new Baltic Sea assistance icebreaker - Railotech",
"url": "https://railotech.fi/news/sweden-orders-new-baltic-sea-assistance-icebreaker/"
},
{
"title": "Baltic Sea icebreakers at capacity this winter - Railotech",
"url": "https://railotech.fi/article/baltic-sea-icebreakers-at-capacity-this-winter/"
},
{
"title": "Ice class",
"url": "https://en.wikipedia.org/wiki/Ice_class"
},
{
"title": "The Swedish forest as a strategic resource for climate, economy, and biodiversity - FOREST EUROPE",
"url": "https://foresteurope.org/the-swedish-forest-as-a-strategic-resource-for-climate-economy-and-biodiversity/"
},
{
"title": "On the distance to recreational forests in Sweden - ScienceDirect",
"url": "https://www.sciencedirect.com/science/article/abs/pii/S0169204600000979"
},
{
"title": "1 The Swedish Forestry Model",
"url": "https://www.ksla.se/wp-content/uploads/2010/10/The-Swedish-Forestry-Model.pdf"
},
{
"title": "New formally protected forest land amounted to 29 200 hectares",
"url": "https://www.scb.se/en/finding-statistics/statistics-by-subject-area/housing-construction-and-building/land-use/formally-protected-forest-land-voluntary-set-asides-consideration-patches-and-unproductive-forest-land/pong/statistical-news/formally-protected-forest-land-voluntary-set-asides-consideration-patches-and-unproductive-forest-land-2022/"
},
{
"title": "Potential Roles of Swedish Forestry in the Context of Climate Change Mitigation",
"url": "https://www.mdpi.com/1999-4907/5/4/557"
},
{
"title": "Sweden Land use - Geography",
"url": "https://www.indexmundi.com/sweden/land_use.html"
},
{
"title": "Sweden Arable land, percent of land area - data, chart",
"url": "https://www.theglobaleconomy.com/Sweden/arable_land_percent/"
},
{
"title": "Agricultural Land in Sweden",
"url": "https://www.worldviewdata.com/countries/sweden/agricultural-land"
},
{
"title": "Is there enough land?",
"url": "https://www.svebio.se/en/is-there-enough-land/"
},
{
"title": "Arable land area",
"url": "https://statbase.org/data/swe-arable-land/"
},
{
"title": "(PDF) Status and restoration of peatlands in northern Europe. Wetlands Ecology and Management, 11, 51-63",
"url": "https://www.researchgate.net/publication/226480989_Status_and_restoration_of_peatlands_in_northern_Europe_Wetlands_Ecology_and_Management_11_51-63"
},
{
"title": "(PDF) The potential peatland extent and carbon sink in Sweden, as related to the Peatland / Ice Age Hypothesis",
"url": "https://www.researchgate.net/publication/234109877_The_potential_peatland_extent_and_carbon_sink_in_Sweden_as_related_to_the_Peatland_Ice_Age_Hypothesis"
},
{
"title": "Forested and Open Wetland Complexes",
"url": "https://link.springer.com/chapter/10.1007/978-1-4615-3524-9_8"
},
{
"title": "Technical Report TR-04-08 Wetlands",
"url": "https://www.osti.gov/etdeweb/servlets/purl/20521180"
},
{
"title": "The Carbon Balance of a Rewetted Minerogenic Peatland Does Not Immediately Resemble That of Natural Mires in Boreal Sweden",
"url": "https://www.ncbi.nlm.nih.gov/pmc/articles/PMC11979567/"
},
{
"title": "1 Mapping of peatlands in the forested landscape of Sweden using",
"url": "https://essd.copernicus.org/preprints/essd-2023-77/essd-2023-77-AR2.pdf"
},
{
"title": "Sweden names 15 Ramsar Sites",
"url": "https://www.ramsar.org/news/sweden-names-15-ramsar-sites"
},
{
"title": "IPS Sweden Post-Convention Excursion 12.-17. June 2025 Mires and peatlands",
"url": "https://peatlands.org/assets/uploads/2025/01/IPS-Post-Convention-Excursion-2025-Sweden-status-april.pdf"
},
{
"title": "Sweden",
"url": "https://en.wikipedia.org/wiki/Sweden"
},
{
"title": "Sweden Population (2026) - Worldometer",
"url": "https://www.worldometers.info/world-population/sweden-population/"
},
{
"title": "North Sweden",
"url": "https://en.wikipedia.org/wiki/North_Sweden"
},
{
"title": "South Sweden",
"url": "https://en.wikipedia.org/wiki/South_Sweden"
},
{
"title": "Stockholm urban area",
"url": "https://en.wikipedia.org/wiki/Stockholm_urban_area"
},
{
"title": "List of metropolitan areas in Sweden",
"url": "https://en.wikipedia.org/wiki/List_of_metropolitan_areas_in_Sweden"
},
{
"title": "Malmö Metropolitan Area (Sweden): Demographic Statistical Areas - Population Statistics, Charts and Map",
"url": "https://www.citypopulation.de/en/sweden/metromalmo/"
},
{
"title": "Malm%C3%B6",
"url": "https://en.wikipedia.org/wiki/Malm%C3%B6"
},
{
"title": "Denmark and Sweden’s cross-border commuters",
"url": "https://ec.europa.eu/regional_policy/sources/communication/boosting_growth/n46_dk_se_commuter_flows.pdf"
},
{
"title": "Futurium",
"url": "https://futurium.ec.europa.eu/en/border-focal-point-network/good-practices/oresund-strategy-denmark-and-swedens-cross-border-commuters?language=el"
},
{
"title": "2.3. Commuting on the Nordic labour market - INSERT NAME OF THE PUBLICATION",
"url": "https://pub.nordregio.org/r-2024-14-nordic-labour-market-70-years/2-3-commuting-on-the-nordic-labour-market.html"
},
{
"title": "OECD Regional Development Working Papers 2013/21 The case of Oresund",
"url": "https://www.oecd.org/content/dam/oecd/en/publications/reports/2013/12/the-case-of-oresund-denmark-sweden-regions-and-innovation-collaborating-across-borders_g17a238e/5k3xv0lk8knn-en.pdf"
},
{
"title": "Swedish History - Hans Högman",
"url": "http://www.hhogman.se/swe_province-county.htm"
},
{
"title": "Svealand",
"url": "https://en.wikipedia.org/wiki/Svealand"
},
{
"title": "Sweden",
"url": "https://www.britannica.com/place/Sweden"
},
{
"title": "Counties of Sweden",
"url": "https://en.wikipedia.org/wiki/Counties_of_Sweden"
},
{
"title": "Regions of Sweden",
"url": "https://en.wikipedia.org/wiki/Regions_of_Sweden"
},
{
"title": "Sweden",
"url": "https://www.arl-international.com/knowledge/country-profiles/sweden"
},
{
"title": "Sweden Map with Counties",
"url": "https://ultimaps.com/vector-maps/europe/sweden-counties/"
},
{
"title": "Provinces of Sweden",
"url": "https://en.wikipedia.org/wiki/Provinces_of_Sweden"
},
{
"title": "Municipalities of Sweden",
"url": "https://en.wikipedia.org/wiki/Municipalities_of_Sweden"
},
{
"title": "Sweden",
"url": "https://terri.cemr.eu/en/country-profiles/sweden.html"
},
{
"title": "Kommunstyrelse",
"url": "https://en.wikipedia.org/wiki/Kommunstyrelse"
},
{
"title": "Sweden's 290 Municipalities - Interactive Map & Complete List",
"url": "https://orti.se/en/municipality"
},
{
"title": "The Swedish Counties (Län)",
"url": "https://www.hhogman.se/swe_counties_map_eng.htm"
},
{
"title": "Sweden's 21 Counties - Complete List, Map & Population",
"url": "https://orti.se/en/county"
},
{
"title": "Snapshot of the SWEDISH FOREST INDUSTRY",
"url": "https://www.skogsindustrierna.se/siteassets/bilder-och-dokument/rapporter/koll-pa-svensk-skogsindustri/snapshot-of-the-swedish-forest-industry-2025.pdf"
},
{
"title": "Forestry - Swedish Forest Industries Federation",
"url": "https://www.forestindustries.se/forest-industry/forest-management/forestry/"
},
{
"title": "Full article: “Profitability is sustainability:” framing of forest management practices by the Swedish forest industry",
"url": "https://www.tandfonline.com/doi/full/10.1080/02827581.2023.2252740"
},
{
"title": "Unasylva - No. 187 - Forest conservation and utilization - The Swedish forest industry in the ecocycle",
"url": "https://www.fao.org/4/w2149e/w2149e04.htm"
},
{
"title": "Facts & figures - Swedish Forest Industries Federation",
"url": "https://www.forestindustries.se/forest-industry/statistics/facts-and-figures/"
},
{
"title": "Kiruna Iron Ore Mine, Sweden - Mining Technology",
"url": "https://www.mining-technology.com/projects/kiruna/"
},
{
"title": "Swedish LKAB Postpones Fossil-Free Sponge Iron Production in Arctic Kiruna",
"url": "https://www.highnorthnews.com/en/swedish-lkab-postpones-fossil-free-sponge-iron-production-arctic-kiruna"
},
{
"title": "Sweden’s LKAB to cut iron ore output at Kiruna mine, production to recover by 2027",
"url": "https://www.steelorbis.com/steel-news/latest-news/swedens-lkab-to-cut-iron-ore-output-at-kiruna-mine-production-to-recover-by-2027-1444571.htm"
},
{
"title": "Kiruna Mine",
"url": "https://www.sika.com/en/reference-projects/kiruna-mine.html"
},
{
"title": "Iron Ore Line",
"url": "https://en.wikipedia.org/wiki/Iron_Ore_Line"
},
{
"title": "Sweden Mining Industry: Legacy and Future",
"url": "https://www.identecsolutions.com/news/sweden-mining-industry-legacy-and-future"
},
{
"title": "Hydropower in Sweden",
"url": "https://www.uniper.energy/sweden/about-uniper-sweden/advantages-hydropower/facts-about-hydropower"
},
{
"title": "Sweden - Towards 100& renewable energy",
"url": "https://www.andritz.com/hydro-en/hydronews/hn-europe/sweden"
},
{
"title": "Advantages of hydropower",
"url": "https://www.uniper.energy/sweden/power-supply-delivers/hydropower-sweden/advantages-hydropower"
},
{
"title": "Unlocking hydropower potential in Sweden: balancing renewable growth and environmental sustainability - International Water Power",
"url": "https://www.waterpowermagazine.com/analysis/unlocking-hydropower-potential-in-sweden-balancing-renewable-growth-and-environmental-sustainability/"
},
{
"title": "Electricity sector in Sweden",
"url": "https://en.wikipedia.org/wiki/Electricity_sector_in_Sweden"
},
{
"title": "More than 100 new nature reserves",
"url": "https://www.scb.se/en/finding-statistics/statistics-by-subject-area/housing-construction-and-building/land-use/protected-nature/pong/statistical-news/protected-nature-2021/"
},
{
"title": "Neglected management of national parks and nature reserves",
"url": "https://www.riksrevisionen.se/en/news-archive/nyhetsarkiv-eng/2024-06-27-neglected-management-of-national-parks-and-nature-reserves.html"
},
{
"title": "Discover untouched wilderness in Sweden’s 30 national parks",
"url": "https://visitsweden.com/what-to-do/nature-outdoors/nature/national-parks/national-parks/"
},
{
"title": "Sweden - Europarc-nb.org",
"url": "https://europarc-nb.org/protected-areas/sweden/"
},
{
"title": "National parks and nature reserves — Naturkartan",
"url": "https://www.naturkartan.se/en/norrbottenslan/articles/nationalparker-och-naturreservat-i-norrbottens-lan"
},
{
"title": "Traditional knowledge and the management of the Laponia World Heritage site",
"url": "https://www.currentconservation.org/traditional-knowledge-and-the-management-of-the-laponia-world-heritage-site-2/"
},
{
"title": "Laponiatjuottjudus: a participatory management system in the Laponian Area World Heritage, Sweden",
"url": "https://panorama.solutions/en/solution/laponiatjuottjudus-participatory-management-system-laponian-area-world-heritage-sweden"
},
{
"title": "Laponian Area - UNESCO World Heritage Centre",
"url": "https://whc.unesco.org/en/list/774/"
},
{
"title": "Postprint - Umeå University - DiVA portal",
"url": "https://umu.diva-portal.org/smash/get/diva2:845848/FULLTEXT01"
},
{
"title": "Laponia - Det Saami culture within the World Heritage Site - Laponia",
"url": "https://laponia.nu/en/det-saami-culture-within-the-world-heritage-site/"
},
{
"title": "Royal Domain of Drottningholm - UNESCO World Heritage Centre",
"url": "https://whc.unesco.org/en/list/559/"
},
{
"title": "The World Heritage Site of Drottningholm - Kungliga slotten",
"url": "https://www.kungligaslotten.se/english/articles-movies-360/drottningholm-palace/2019-08-25-the-world-heritage-site-of-drottningholm.html"
},
{
"title": "Drottningholm Palace",
"url": "https://en.wikipedia.org/wiki/Drottningholm_Palace"
},
{
"title": "World Heritage Photos - Royal Domain of Drottningholm",
"url": "https://www.werelderfgoedfotos.nl/en/photos/49-royal-domain-of-drottningholm.html"
},
{
"title": "whc.unesco.org",
"url": "https://whc.unesco.org/document/216943"
},
{
"title": "Why the Baltic Sea still chokes after decades of nutrient controls",
"url": "https://phys.org/news/2026-02-baltic-sea-decades-nutrient.html"
},
{
"title": "State of the Baltic Sea 2026: Facts, pollution and solutions",
"url": "https://www.raceforthebaltic.com/baltic-sea"
},
{
"title": "Explainer: What Is a Dead Zone?",
"url": "https://earth.org/what-is-a-dead-zone/"
},
{
"title": "Focus on oxygen depletion in the Baltic Sea",
"url": "https://www.meere-online.de/en/topics/pollution/translate-to-english-fokus-sauerstoffmangel-in-der-ostsee"
},
{
"title": "Rapid re-oxygenation of Baltic Sea sediments following a large inflow event",
"url": "https://www.ncbi.nlm.nih.gov/pmc/articles/PMC4709353/"
},
{
"title": "www.frontiersin.org",
"url": "https://www.frontiersin.org/journals/marine-science/articles/10.3389/fmars.2021.799936/pdf"
},
{
"title": "The Baltic Sea is suffocating: on eutrophication, european farmers and agricultural policies",
"url": "https://voxeurop.eu/en/baltic-sea-suffocating-eutrophication-agriculture/"
},
{
"title": "Can oxygen pump breathe life into ocean 'dead zone?'",
"url": "https://www.cnn.com/2012/07/17/world/europe/dead-zone-baltic-oxygen"
},
{
"title": "Can deep-water Oxygenation bring back life into Baltic ‘dead zones’?",
"url": "https://sustainablebaltic.wordpress.com/2016/07/21/can-deep-water-oxygenation-bring-back-life-into-baltic-dead-zones/"
},
{
"title": "The Swedish Red List 2025",
"url": "https://researchdata.se/en/catalogue/dataset/2026-63"
},
{
"title": "Analysis: A Closer Look at Biodiversity Loss in Sweden",
"url": "https://naturereclamation.substack.com/p/analysis-a-closer-look-at-biodiversity"
},
{
"title": "Investigation: Sweden's Old-Growth Forest Crisis",
"url": "https://naturereclamation.substack.com/p/investigation-swedens-old-growth"
},
{
"title": "1 Biodiversity in the forests",
"url": "https://www.forestindustries.se/siteassets/bilder-och-dokument/rapporter/biologisk-mangfald/skogs_rapport_bio_eng_final_links-1.pdf"
},
{
"title": "Biodiversity and our responsibility - Swedish Wood",
"url": "https://www.swedishwood.com/sustainability/forest/biodiversity-and-our-responsibility/"
},
{
"title": "(PDF) The new Swedish Red List 2010",
"url": "https://www.researchgate.net/publication/279761923_The_new_Swedish_Red_List_2010"
},
{
"title": "Swedish Government Official Reports Sweden facing climate change",
"url": "https://www.government.se/contentassets/5f22ceb87f0d433898c918c2260e51aa/sweden-facing-climate-change-sou-200760/"
},
{
"title": "Climate warming shortens ice durations and alters freeze and break-up patterns in Swedish water bodies",
"url": "https://repository.library.noaa.gov/view/noaa/58143"
},
{
"title": "Experimentally increased snow depth affects high Arctic microarthropods inconsistently over two consecutive winters",
"url": "https://www.ncbi.nlm.nih.gov/pmc/articles/PMC9613649/"
},
{
"title": "Terrestrial Arthropod Responses to Arctic Cryosphere Degradation - PMC",
"url": "https://pmc.ncbi.nlm.nih.gov/articles/PMC13478772/"
},
{
"title": "Effects of Climate Change in Sweden",
"url": "https://www.osti.gov/etdeweb/servlets/purl/392699"
},
{
"title": "Keeping pace with forestry: Multi-scale conservation in a changing production forest matrix",
"url": "https://www.ncbi.nlm.nih.gov/pmc/articles/PMC7067752/"
}
],
"license": "https://creativecommons.org/licenses/by/4.0/"
}