This articleneeds additional citations forverification. Please helpimprove this article byadding citations to reliable sources. Unsourced material may be challenged and removed. Find sources: "Climate of Norway" – news ·newspapers ·books ·scholar ·JSTOR(December 2023) (Learn how and when to remove this message)

Theclimate of Norway is more temperate than expected for highlatitudes. This is mainly due to theNorth Atlantic Current with its extension, theNorwegian Current, raising the air temperature;^[1] the prevailing southwesterlies bringing mild air onshore; and the general southwest–northeast orientation of the coast, which allows the westerlies to penetrate into theArctic. The January average inBrønnøysund^[2] is 15 °C (59 °F) higher than the January average inNome, Alaska,^[3] even though both towns are situated on the west coast of the continents at 65°N. In July the difference is reduced to 3.2 °C (37.8 °F). The January average ofYakutsk, inSiberia but slightly further south, is −42.3 °C (−44.1 °F) lower than in Brønnøysund.^[4]

Norway is among Europe's wettest countries, but with large variation in precipitation amount due to the terrain with mountain chains resulting in orographic precipitation but also creating rain shadows. In some regions, locations with vastly different precipitation amounts can be fairly close.Stryn Municipality (1661 mm) get 6 times as much precipitation as Skjåk 90 minutes drive away, Bergen has five times as much precipitation asLærdal Municipality in the same region, and in the northGlomfjord (2141 mm) get 10 times as much precipitation as upper Saltdal (81 m) which is 68 km away as the crow flies. Some areas of Vestlandet and southern Nordland are among Europe's wettest, due toorographic lift, particularly where thewesterlies are first intercepted by high mountains. This occurs slightly inland from the outer skerry guard. In the updated 1991-2020 normals,Gullfjellet in Bergen (345 m) has the highest annual precipitation with 4,067 mm (160.1 in). Annual precipitation can exceed 5,000 mm (196.9 in) in mountain areas near the coast.Lurøy Municipality at the Arctic Circle gets 3,066 mm (120.7 in) annually, a remarkable amount for a polar location. Precipitation is heaviest in late autumn and winter along the coast, while April to June is the driest.The innermost parts of the long fjords are somewhat drier: annual precipitation inLærdal Municipality is 514 mm (20.2 in), and in the north only 338 mm (13.3 in) inSkibotn at the head ofLyngenfjord.

The regions east of the mountain chain (includingOslo) have a more continental climate with generally less precipitation, and precipitation peaks in summer and early autumn, while winter and spring tend to be driest. A large area in the interior of Finnmark receive less than 450 mm (17.7 in) of precipitation annually. Some valleys surrounded by mountains get very scarce precipitation, and often need irrigation in summer. The upper part ofSaltdal Municipality (81 m,Storjord) has the lowest annual average with only 211 mm (8.3 in), while in the south of Norway,Skjåk Municipality is driest with 295 mm (11.6 in). In Norway's High Arctic archipelagoes,Svalbard Airport has the lowest average annual precipitation with 217 mm (8.5 in), whileJan Mayen get more than double with 648 mm (25.5 in).

Monthly averages vary from 6 mm (0.24 in) in April in upper Saltdal and Skjåk to 509 mm (20.0 in) in December at Gullfjellet. Coastal areas fromLindesnes Municipality north toVardø Municipality have more than 200 days per year with precipitation; however, this is with a very low threshold value (0.1 mm precipitation). The average annual number of days with at least 3 mm (0.12 in) precipitation is 77 in Blindern/Oslo, 96 in Kjevik/Kristiansand, 158 in Florida/Bergen, 93 in Værnes/Trondheim, and 109 inTromsø.^[5]

The coast experiences milder winters than other areas at the same latitudes. The average temperature difference between the coldest month and the warmest is only 10–15 °C (18–27 °F) in coastal areas; some lighthouses have a yearly amplitude of just 10 °C (18 °F), such as Svinøy inHerøy Municipality with a coldest month of 3.7 °C (38.7 °F). The differences of inland areas are larger, with a maximum difference of 28 °C (50 °F) inKarasjok Municipality.Finnmarksvidda has the coldest winters in mainland Norway, but inland areas much further south can also experience severe cold.Røros Municipality has recorded −50 °C (−58 °F).

Bø Municipality is the most northerly location in the world where all winter months have mean temperatures above 0 °C (32 °F). 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 nighttime temperatures differ the most. Inland valleys and the innermost fjord areas have less wind and see the warmest summer days. The lowland near Oslo is warmest in summer with 24 July-hr average of 18 °C (64.4 °F) and average daily high up to 23 °C (73.4 °F). Inland areas reach their peak warmth 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 over the northern part of the Norwegian Sea, one branch going east into the Barents Sea and the other going north along the west coast ofSpitsbergen. This modifies the Arcticpolar climate somewhat and results in open water throughout the year at higherlatitudes than any other place in the Arctic. On the eastern coast of theSvalbardarchipelago, the sea used to be frozen during most of the year, but the last years' warming (graph) have seen open waters noticeably longer.

The warmest temperature ever recorded in Norway is 35.6 °C (96.1 °F) inNesbyen Municipality. The coldest temperature ever is −51.4 °C (−60.5 °F) inKarasjok Municipality. The warmest month on record was July 1901 in Oslo, with a mean 24-hour temperature of 22.7 °C (72.9 °F)), and the coldest month was February 1966 in Karasjok, with a mean of −27.1 °C (−16.8 °F). The warmest night recorded in Norway was July 29, 2019 at Sømna-Kvaløyfjellet (302 m) inSømn Municipalitya near Brønnøysund with overnight low 26.1 °C (79.0 °F).^[6] Atlantic lows bringing mild winds in winter further warmed byfoehn can give warm temperatures in narrow fjords in winter:Sunndalsøra has recorded 19 °C (66 °F) in January and 18.9 °C (66.0 °F) in February.

Compared to coastal areas, inland valleys and the innermost fjord areas have largerdiurnal temperature variations, especially in spring and summer.

Areas in Norway located north of theArctic Circle haveextreme darkness in winter, which increases withlatitude. AtLongyearbyen on the Svalbard islands in the extreme north, the upper part of the sun's disc is above the horizon from 9 April to 23 August, and winter darkness lasts from 27 October to 14 February. The winter darkness is not as dark on the northern mainland, as there istwilight for a few hours around noon.

The southern part of the country also experiences large seasonal variations in daylight; in Oslo, the sun rises at 03:54 and sets 22:54 at thesummer solstice, but is only above the horizon from 09:18 to 15:12 at thewinter solstice. The northern part of the country is located in theaurora borealis zone; the aurora is occasionally seen in the southern part of the country as well.

Norway is onCentral European Time, corresponding to the15°E longitude. As the country is very elongated, this is at odds with the local daylight hours in the eastern and western parts. In Vardø, local daylight hours are 64 minutes earlier, and in Bergen, they are 39 minutes later. Thus, Finnmark gains early morning daylight but loses evening daylight, andVestlandet loses early morning light but gains more evening daylight in this time zone.Daylight saving time (GMT + 2) is observed from the last Sunday in March to the last Sunday in October.

The difference between lowtide and high tide is small on the southern coast and large in the north; ranging from on average 0.17 m inMandal to about 0.30 m in Oslo and Stavanger, 0.90 m in Bergen, 1.80 m in Trondheim, Bodø and Hammerfest and as much as 2.17 m inVadsø.

As seen from the table, Norway's climate shows large variations, but all populated areas of the Norwegian mainland have temperate or subarctic climates (Köppen groupsC andD). Svalbard and Jan Mayen have a polar climate (Köppen groupE).

As a consequence of warming since 1990, summers are warmer and longer and winters are getting shorter and milder. With the new official 1991-2020 climate normal, many areas have seen their climate change to a new climate zone compared to 1961-90 normal. Oslo's climate has moved from Dfb to Cfb/Dfb, Lillehammer's from Dfc to Dfb, Kristiansand from Cfb/Dfb to Cfb, Molde and Brønnøysund from Cfc/Dfc to Cfb, Trondheim from Dfc to Cfb/Dfb, Bodø from Cfc/Dfc to Cfb/Dfb, Tromsø (Holt) from Dfc to Cfc/Dfc and Vardø from ET to Dfc. Snow cover has decreased in most populated areas due to winter warming; days/year with 25 cm snow cover in 1991-2020 is 26 days in Oslo (94 m), 2 days in Bergen, 8 days in Trondheim/Værnes and 144 days in Tromsø. The strongest warming has been observed on Svalbard. In addition to warming, precipitation has increased in most areas, especially in winter, increasingerosion and the risk oflandslides.

This section is an excerpt fromClimate change in Norway.[edit]

All regions and seasons ofNorway are expected tobecome warmer and wetter due toclimate change.

On aper-capita basis, Norway is the world's largest producer, and exporter, ofoil and natural gas outside theMiddle East.^[31] In 2016, 56 new licenses foroil exploration near theLofoten Islands were issued. However, 98% of Norway's electricity demand is supplied byrenewable sources, mostly fromhydroelectric power, generated using Norway's extensive freshwater reserves.^[32] Emissions are also generated through transportation, although Norway is a world leader inelectric vehicles.

Warmer temperatures in Norway are causingpermafrost andglaciers to retreat, and leading to shifts in precipitation patterns.Climate change is particularly impacting Norway'sArctic region.Biodiversity and forested areas are experiencing shifts due to the phenomenon, with significant implications for theagriculture and economy of the country. IndigenousSámi people's practices are being impacted by climate change.

Norway's government have introduced several social and economic policies towardsclimate change mitigation, including throughcarbon capture and storage. Norway wants to achievecarbon neutrality by 2030, partly by investing in projects with emissions reduction abroad. It wants to achieve zero emission in the country by 2050.^[33] In 2020, Norway pledged to achieve a 50% - 55% reduction in domestic emissions from the level of 1990 by 2030.^[34]

• Climate
• Geography of Norway

• Climate of Norway
• Climate by country

• CS1 Norwegian-language sources (no)
• Articles with short description
• Short description is different from Wikidata
• Articles needing additional references from December 2023
• All articles needing additional references
• Articles with excerpts