Scandinavia - Geography

Geography

See also: Geography of Denmark, Geography of Finland, Geography of Iceland, Geography of Norway, and Geography of Sweden

The geography of Scandinavia is extremely varied. Notable are the Norwegian fjords, the Scandinavian Mountains, the flat, low areas in Denmark, and the archipelagos of Sweden and Norway. Sweden has many lakes and moraines, legacies of the ice age.

The climate varies from north to south and from west to east; a marine west coast climate (Cfb) typical of western Europe dominates in Denmark, southernmost part of Sweden and along the west coast of Norway reaching north to 65°N, with orographic lift giving more mm/year precipitation (<5000 mm) in some areas in western Norway. The central part – from Oslo to Stockholm – has a humid continental climate (Dfb), which gradually gives way to subarctic climate (Dfc) further north and cool marine west coast climate (Cfc) along the northwestern coast. A small area along the northern coast east of the North Cape has tundra climate (Et) as a result of a lack of summer warmth. The Scandinavian Mountains block the mild and moist air coming from the southwest, thus northern Sweden and the Finnmarksvidda plateau in Norway receive little precipitation and have cold winters. Large areas in the Scandinavian mountains have alpine tundra climate.

The warmest temperature ever recorded in Scandinavia is 38.0 °C in Målilla (Sweden). The coldest temperature ever recorded is −52.6 °C in Vuoggatjålme (Sweden). The warmest month on record was July 2010 in Puumala, Finland, with a mean (24hr) of 23.0 °C, and the coldest month was February 1985 in Vittangi (Sweden) with a mean of −27.2 °C.

Southwesterly winds further warmed by foehn wind can give warm temperatures in narrow Norwegian fjords in winter; Tafjord has recorded 17.9 °C in January and Sunndal 18.9 °C in February.

Scandinavia is still recovering from the last Ice Age, when ice depressed the land by 2000 ft (600 m). This gradual uplift is known as isostatic rebound.