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Climate change has received significant scientific, public and political attention in Sweden. In 1896, Swedish chemist Svante Arrhenius was the first scientist to quantify global heating . [ 12 ] Sweden has a high energy consumtion per capita, but reducing the dependency on fossil energy has been on the agenda of cabinets of the Governments of ...
Map of Sweden. Much of Sweden is heavily forested, with 69% [1] of the country being forest and woodland, while farmland constitutes only 8% of land use. [2] Sweden consists of 39,960 km 2 of water area, constituting around 95,700 lakes. [3] [A] The lakes are sometimes used for water power plants, especially the large northern rivers and lakes.
The Köppen climate classification system was modified further within the Trewartha climate classification system in 1966 (revised in 1980). The Trewartha system sought to create a more refined middle latitude climate zone, which was one of the criticisms of the Köppen system (the climate group C was too general). [10]: 200–1
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Map of Sweden's five major vegetation zones. Sweden has a considerable south to north distance which causes large climatic difference, especially during the winter. The related matter of the length and strength of the four seasons plays a role in which plants that naturally can grow at various places. Sweden is divided into five major ...
Geography of Sweden. Sweden is: a Nordic country; Location: The regions that Sweden is located in are: Northern Hemisphere and Eastern Hemisphere; Eurasia. Europe. Northern Europe. Scandinavia. Scandinavian Peninsula; Time zone: Central European Time , Central European Summer Time ; Extreme points of Sweden. High: Kebnekaise 2,104 m (6,903 ft)
Today, the most commonly used climate map is the Köppen climate classification, developed by Russian climatologist of German descent and amateur botanist Wladimir Köppen (1846–1940), which divides the world into five major climate regions, based on average annual precipitation, average monthly precipitation, and average monthly temperature.
The climate and ecology of different locations on the globe naturally separate into life zones, depending on elevation, latitude, and location. The generally strong dependency on elevation is known as altitudinal zonation : the average temperature of a location decreases as the elevation increases.