Climate
The climate of Norway is surprisingly temperate for such a northerly country; this is mainly due to the North Atlantic Current with its extension the Norwegian Current warming the air temperature, and the prevailing southwesterlies bringing the mild air on shore.
Temperature
The coast experiences much milder winters than other areas at the same latitudes. The islands in southern Lofoten, to the north of the Arctic Circle in North Norway, are the most northerly locations in the world where all winter months have mean temperatures above 0°C. Finnmarksvidda has the coldest winters in Norway, but inland areas further south can also see severe cold; Røros has recorded -50°C. Spring is the season when the temperature differences between the southern and northern part of the country is largest; this is also the time of year when daytime and night-time temperatures differs the most. Inland vallys and the innermost fjord areas have less wind and sees the warmest summer days; the Oslofjord lowland is warmest with July 24-hr average of 17°C, but even Alta at 70°N has July average of 13.5°C, and commercial fruit orchards are common in the innermost areas of the western fjords. Inland areas reach their warmth peak around mid-July, and coastal areas by the first half of August. Humidity is usually low in summer.
The North Atlantic Current splits in two in the northern part of the Norwegian Sea; one branch goes east into the Barents Sea, while the other goes north along the west coast of Spitsbergen; this modifies the Arctic polar climate somewhat and results in open water throughout the year at higher latitudes than any other place in the Arctic. On the eastern coast of the Svalbard archipelago, the sea used to be frozen during most of the year, but the last years warming (graph) have seen open waters noticeably longer.
Normal monthly averages range from -17.1°C in January in Karasjok to 17.3°C in July in Oslo - Studenterlunden. The warmest year average temperature is 7.7°C in Skudeneshavn in Karmøy, and the coldest is -3.1°C in Sihcajarvi in Kautokeino (excluding higher mountains and Svalbard); this is a 10.8°C difference, about the same as the temperature difference between Skudeneshavn and Athens, Greece.
The warmest temperature ever recorded in Norway is 35.6°C in Nesbyen. The coldest temperature ever recorded is -51.4°C in Karasjok. The warmest month on record was July 1901 in Oslo, with a mean (24hr) of 22.7°C, and the coldest month was February 1966 in Karasjok with a mean of -27.1°C. Southwesterly winds further warmed by foehn can give warm temperatures in narrow fjords in winter; Tafjord has recorded 17.9°C in January and Sunndal 18.9°C in February.
Average daily minimum temperature in January is -6.8°C in Oslo, -4.8°C in Kristiansand, -0.4°C in Bergen and -6.5°C in Trondheim and Tromsø. The average daily high in July is 21.5°C in Oslo, 20.1°C in Kristiansand, 17.6°C in Bergen, 18.4°C in Trondheim and 15.3°C in Tromsø.
Precipitation
Some areas of Vestlandet and southern Nordland are Europe's wettest due to orographic lift, particularly where the moist westerlies first are intercepted by high mountains; this occurs slightly inland from the outer skerry guard. Brekke in Sogn og Fjordane has the highest annual precipitation with 3,575 mm; annual precipitation can exceed 5,000 mm in mountain areas near the coast. Lurøy, near the Arctic Circle, gets 2,935 mm on average, an amazing humidity for such a northerly area.
Precipitation is heaviest in autumn and early winter along the coast, while April to June is the driest. The innermost parts of the long fjords are somewhat drier, annual precipitation in Lærdal is 491 mm, in Levanger 750 mm and only 300 mm in Skibotn at the head of Lyngenfjord, the latter also has the national record for clear-weather days.
The regions to the east of the mountains (including Oslo) have a more continental climate with less precipitation, and enjoys more sunshine and usually warmer summers; precipitation is highest in summer and early autumn (often heavy showers not lasting long) while winter and spring tend to be driest inland. Valleys surrounded by mountains can be very dry compared to nearby areas, and a larger area in the interior of Finnmark gets less than 400 mm precipitation annually. Svalbard Airport has the lowest average annual precipitation with 190 mm, while Skjåk has the lowest average on the mainland with only 278 mm, the lowest ever recorded on the mainland is 64 mm at Hjerkinn in Dovre.
Monthly averages varies from 5 mm in April in Skjåk to 454 mm in September in Brekke. Coastal areas from Lindesnes north to Vardø have more than 200 days/year with precipitation; however this is with a very low threshold value (0.1 mm precipitation). Average number of days/year with at least 3 mm precipitation is 77 in Blindern/Oslo, 96 in Kjevik/Kristiansand, 158 in Florida/Bergen, 93 in Værnes/Trondheim and 109 in Tromsø.
| Location | Elevation | Jan (°C) | July (°C) | Year (°C) | Annual Precipitation |
|---|---|---|---|---|---|
| Bardufoss | 76 m | -10.4 | 13.0 | 0.7 | 652 mm |
| Blindern/Oslo | 94 m | -4.3 | 16.4 | 5.7 | 763 mm |
| Bolna in Rana/Saltfjell | 549 m | -11.1 | 10.8 | -0.4 | 990 mm |
| Florida/Bergen | 12 m | 1.3 | 14.3 | 7.6 | 2250 mm |
| Geilo | 810 m | -8.2 | 11.2 | 1.0 | 700 mm |
| Honningsvåg | 10 m | -4.5 | 10.3 | 2.0 | 765 mm |
| Kirkenes | 10 m | -11.5 | 12.6 | -0.2 | 450 mm |
| Kristiansand | 22 m | -0.9 | 15.7 | 7.0 | 1380 mm |
| Lærdal | 24 m | -2.5 | 14.7 | 5.9 | 491 mm |
| Langnes/Tromsø | 8 m | -3.8 | 11.8 | 2.9 | 1000 mm |
| Lillehammer | 242 m | -9.1 | 14.7 | 2.9 | 660 mm |
| Longyearbyen/Svalbard | 28 m | -14.6 | 6.5 | -6.0 | 210 mm |
| Molde | 20 m | 0.5 | 13.5 | 6.7 | 1640 mm |
| Rørvik | 25 m | -0.9 | 12.8 | 5.6 | 1285 mm |
| Sognefjellhytta/Lom | 1413 m | -10.7 | 5.7 | -3.1 | 860 mm |
| Sola/Stavanger | 7 m | 0.8 | 14.2 | 7.4 | 1180 mm |
| Svolvær/Lofoten | 10 m | -1.5 | 13.0 | 4.7 | 1500 mm |
| Tønsberg | 10 m | -3.2 | 16.8 | 6.3 | 930 mm |
| Værnes/Trondheim | 12 m | -3.4 | 13.7 | 5.0 | 892 mm |
As seen from the table above, Norway's climate shows large variations:
- maritime mild temperate / marine west coast climate as in Bergen
- hemiboreal / humid continental as in Oslo
- cool maritime as in Svolvær
- continental subarctic climate as in Kirkenes
- polar tundra as in Longyearbyen (a narrow area along the northeastern coast from Nordkapp to Vardø are also polar tundra)
In addition, large mountain areas have alpine tundra climates. True ice cap climate can be found at elevations higher than approximately 400 - 800 m in Svalbard and Jan Mayen, lowest on Nordaustlandet.
Global Warming
Temperatures have tended to be higher in recent years, with average January temperatures for the same stations that are 1 °C to 2.5 °C higher than those found before 1991, while the July 24-hr average temperatures have increased by approximately 0.5 to 1 °C.
As a consequence of warming, summers last longer and winters are getting shorter; snow cover have tended to decrease in those lowland areas where winter temperatures often hover around freezing (including most major cities), while winter precipitation in the mountains and cold inland areas still falls as snow. The strongest warming has been observed on Svalbard. In addition to warming, precipitation have increased on the mainland, especially in autumn and winter.
