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The coastal lowlands of Iceland have average January temperatures of about 0 °C (32 °F), while the highlands of central Iceland generally stay below −10 °C (14 °F). The lowest winter temperatures in Iceland are usually somewhere between −25 °C (−13 °F) and −30 °C (−22 °F), although the lowest temperature ever recorded on ...
The South Swedish highlands have been populated since the Nordic Stone Age as evidenced by cist findings. [6] During the Nordic Bronze Age (c. 1700 –500 BC) there was a significant agricultural expansion across the highlands.
A composed satellite photograph of islands and continental areas in and surrounding the North Sea and Baltic Sea.. The northern region of Europe has several definitions. A restrictive definition may describe northern Europe as being roughly north of the southern coast of the Baltic Sea, which is about 54°N, or may be based on other geographical factors such as climate and ecology.
Further north, large areas in the interior highlands or uplands of Trøndelag and North Norway are dominated by the NB zone, with the tree line at about 800 metres (2,600 ft) amsl in the interior of Trøndelag, 600 metres (2,000 ft) in Rana Municipality, 500 metres (1,600 ft) at Narvik, 400 metres (1,300 ft) at Tromsø, 200 metres (660 ft) at ...
The Scandinavian Mountains or the Scandes is a mountain range that runs through the Scandinavian Peninsula.The western sides of the mountains drop precipitously into the North Sea and Norwegian Sea, forming the fjords of Norway, whereas to the northeast they gradually curve towards Finland.
Constant precipitation throughout the year, no dry season. Its temperature oscillates between 10 °C and 20 °C. Precipitation is higher than other highlands, about 1500 mm. It is the tropical variation of the oceanic climate Cfb. It can appear anywhere within the tropical zone with much rainfall and adequate altitude. Cities:
Met Office warns of ‘significant disruption’ to transport, power lines and phone network coverage
The temperature profile of the atmosphere is a result of an interaction between radiation and convection.Sunlight in the visible spectrum hits the ground and heats it. The ground then heats the air at the surface.