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- W61624541 abstract "Fennoscandia is strongly influenced by the warm Gulf Stream along the coast of Norway causing higher temperatures than in other parts of the world at similar latitudes (about 60–70° N). Most of the tundra (defined as areas with annual mean air temperatures below 0° C) in Fennoscandia is alpine (about 50% of Norway as a whole). The annual mean temperature is -1 to -2° C at 1200 m in the southwestern parts about 200 m above the tree line and is as low as about 0° C even in the upper birch forest zone. Tundra areas close to sea level are only found in the northernmost regions. Annual mean temperatures in the birch forest at Kevo, northern Finland, about 100 m above sea level, are about -2° C (Kallio, 1975). The dominating westerly winds and the Fennoscandian mountain range north-south through most of Norway in western Fennoscandia cause high precipitation in the west, and leaside effects east of the mountains. At the mountain plateau, Hardangervidda, in southern Norway, annual precipitation decreases for instance from above 1500 mm in the west to about 500 mm in the east (Østbye et al., 1975), while only about 300 mm per year is registered at Abisko, northern Sweden, just east of the mountain range (Rosswall et al., 1975 b). Permafrost is only found in peaty soil in northern parts of Fennoscandia with moderate winter precipitation. Polar days (midnight sun) last for more than two months in the north (e.g. the Kevo area) while day length never exceeds about 20 hrs in southern Fennoscandia." @default.
- W61624541 created "2016-06-24" @default.
- W61624541 creator A5044827130 @default.
- W61624541 date "1975-01-01" @default.
- W61624541 modified "2023-10-16" @default.
- W61624541 title "Functioning of Fennoscandian Tundra Ecosystems" @default.
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- W61624541 doi "https://doi.org/10.1007/978-3-642-66276-8_36" @default.
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