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Skrova lighthouse on an island near Svolvær has the longest recording of air temperature in Lofoten. The warmest temperature recorded is 30.4 °C (86.7 °F) in June 1972. The coldest temperature recorded is −15.1 °C (4.8 °F) in February 1966. The last overnight freeze in June was in 1962, and the last freeze in September was in 1986.
If the annual precipitation is less than 50% of this threshold, the classification is BW (arid: desert climate); if it is in the range of 50%–100% of the threshold, the classification is BS (semi-arid: steppe climate). [9] [11] A third letter can be included to indicate temperature.
The southerly lowlands of the island average around 0 °C (32 °F) in winter, while the north averages around −10 °C (14 °F). The lowest temperatures in the northern part of the island range from around −25 to −30 °C (−13 to −22 °F). The lowest temperature on record is −39.7 °C (−39.5 °F). [4]
The thermohaline circulation affects the climate in the Norwegian Sea, and the regional climate can significantly deviate from average. There is also a difference of about 10 °C between the sea and the coastline. Temperatures rose between 1920 and 1960, [19] and the frequency of storms decreased in this period. The storminess was relatively ...
Average January temperatures range from about −40 to 0 °C (−40 to 32 °F), and winter temperatures can drop below −50 °C (−58 °F) over large parts of the Arctic. Average July temperatures range from about −10 to 10 °C (14 to 50 °F), with some land areas occasionally exceeding 30 °C (86 °F) in summer.
Northern parts of Finland have summer temperatures in the 8 °C (46 °F) to 16 °C (61 °F) range, while further south, the temperature is closer to 13 °C (55 °F) and 23 °C (73 °F). [ 9 ] [ 10 ] During summer in Greenland , ice sheets breaking up trigger what is known as " glacial motion " or "glacial earthquakes".
Through the eddy activity of the Lofoten Basin and the persistence of the Lofoten Vortex, the residence time of the warm water is lengthened, leading to additional cooling of the AW before it reaches the Arctic Ocean. [4] Due to heat loss, the temperature decreases and the light-to-dense water transformation takes place.
Regions where oceanic or subtropical highland climates (Cfb, Cfc, Cwb, Cwc) are found. An oceanic climate, also known as a marine climate or maritime climate, is the temperate climate sub-type in Köppen classification represented as Cfb, typical of west coasts in higher middle latitudes of continents, generally featuring cool to warm summers and cool to mild winters (for their latitude), with ...