Scandinavia

Lore & Background

During the Viking Age Scandinavian peoples participated in large-scale raiding, conquest, colonization and trading mostly throughout Europe. They also used their longships for exploration, becoming the first Europeans to reach North America. These exploits saw the establishment of the North Sea Empire which comprised large parts of Scandinavia and Great Britain, though it was relatively short-lived. Scandinavia was eventually Christianized, and the coming centuries saw various unions of Scandinavian nations, most notably the Kalmar Union of Denmark, Norway and Sweden, which lasted for over 100 years until the Swedish king Gustav I led Sweden out of the union.

Denmark and Norway, as well as Schleswig-Holstein, were then united until 1814 as Denmark–Norway. Numerous wars between the nations followed, which shaped the modern borders and led to the establishment of the Swedish Empire in the 17th and early 18th centuries. The most recent Scandinavian union was the union between Sweden and Norway, which ended in 1905.

Reader's Guide

The geography of Scandinavia is extremely varied. Notable are the Norwegian fjords, the Scandinavian Mountains covering much of Norway and parts of Sweden, the flat, low areas in Denmark and the archipelagos of Finland, Norway and Sweden. Finland and Sweden have many lakes and moraines, legacies of the ice age, which ended about ten millennia ago. The southern regions of Scandinavia, which are also the most populous regions, have a temperate climate.

Scandinavia extends north of the Arctic Circle, but has relatively mild weather for its latitude due to the Gulf Stream. Many of the Scandinavian mountains have an alpine tundra climate. 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, the 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.

Did You Know?

• The warmest temperature ever recorded in Scandinavia is 38.0°C in Målilla (Sweden).
• The coldest temperature ever recorded is −52°C in Vuoggatjålme, Arjeplog (Sweden).
• The coldest month was February 1985 in Vittangi (Sweden) with a mean of −27.2°C.