Climate of Finland

File:Koppen-Geiger Map v2 FIN 1991–2020.svg

Köppen climate classification types of Finland

The climate of Finland is influenced most by its latitude: Finland is located between 60 and 70 N. Because of Finland's northern location, winter is the longest season. Only on the south coast and in the southwest is summer as long as winter. On average, winter lasts from early December to late March along the southern coast and from early October to mid May in the northernmost locations such as Lapland. This means that southern portions of the country are snow-covered about three to four months of the year, and the northern for about seven months. The long winter causes about half of the annual precipitation in the north to fall as snow. Precipitation in the south amounts to about annually. Like that of the north, it occurs all through the year, though not so much of it is snow.

In Köppen climate classification Finland belongs to the Df group (continental subarctic or boreal climates). The southern coast is Dfb (humid continental mild summer, wet all year), and the rest of the country is Dfc (subarctic with cool summer, wet all year).

The climate of Finland has characteristics of both maritime and continental climate. The Atlantic Ocean to the west and the Eurasian continent to the east interact to modify the climate of the country. The warm waters of the Gulf Stream and the North Atlantic Drift Current, which continuously warm the region, play a big role in the climate of Norway, Sweden and Finland; if it weren't for these currents, the winters in Scandinavia and Fennoscandia would be much colder. Westerly winds bring the warm air currents into the Baltic areas and to the country's shores, moderating winter temperatures, especially in the south and southwest in cities like Helsinki and Turku where winter highs tend to be between but a cold snap like the one that occurred in mid-January 2016 can cause temperatures to plunge well below . These winds, because of clouds associated with weather systems accompanying the westerlies, also decrease the amount of sunshine received during the summer. By contrast, the continental high pressure system situated over the Eurasian continent counteracts the maritime influences, occasionally causing severe winters and high temperatures in the summer.

Temperature

The warmest annual average temperature in Southwestern Finland is . From there the temperature decreases gradually towards north and east. The Suomenselkä and Maanselkä drainage divides rise higher than the surrounding areas, and the climate there is cooler than at same latitudes elsewhere in Finland. The Barents Sea between Finland and the North Pole is open even in winter, so northerly airflows are not as cold as in Siberia or Alaska.

The highest temperature ever recorded is (Liperi, July 29, 2010). The lowest, (Kittilä, January 28, 1999). The annual average temperature is relatively high in the southwestern part of the country (), with quite mild winters and warm summers, and low in the northeastern part of Lapland (Finland) ().

Temperature extremes for every month:

Record highs and lows

Record highs by month
Month	Temp.	Date	Location
January		January 6, 1973	Mariehamn, Åland
February		February 28, 1943	Ilmala, Helsinki, Uusimaa
March		March 27, 2007	Helsinki-Vantaa Airport, Vantaa, Uusimaa
April		April 27, 1921	Jyväskylä, Central Finland
May		May 30/31, 1995	Lapinjärvi, Uusimaa
June		June 24, 1934	Ähtäri, South Ostrobothnia
July		July 29, 2010	Joensuu Airport, Liperi, North Karelia
August		August 7, 2010	Heinola, Päijät-Häme, Puumala, South Savo
		August 8, 2010	Lahti, Päijät-Häme
September		September 6, 1968	Rauma, Satakunta
October		October 14, 2018	Oulu Airport, North Ostrobothnia
November		November 6, 2020	Mariehamn Airport, Jomala, Åland
December		December 20, 2015	Pori and Kokemäki, Satakunta

Record lows by month
Month	Temp.	Date	Location
January		January 28, 1999	Kittilä, Pokka, Lapland
February		February 5, 1912	Sodankylä, Lapland
March		March 1, 1971	Salla, Tuntsa, Lapland
April		April 2/9, 1912	Kuusamo, Northern Ostrobothnia; Sodankylä, Lapland
May		May 1, 1971	Enontekiö, Kalmankaltio, Lapland
June		June 1, 2023	Saana, Kilpisjärvi, Enontekiö, Lapland
July		July 1/12, 1958	Enontekiö, Kilpisjärvi, Lapland
August		August 26, 1980	Salla, Naruskajärvi, Lapland
September		September 26, 1968	Sodankylä, Vuotso, Lapland
October		October 25, 1968	Sodankylä, Lapland
November		November 30, 1915	Sodankylä, Lapland
December		December 21, 1919	Pielisjärvi, North Karelia

• Measurements are made at the height of 2 metres. A record cold of sorts for June, was measured on June 2, 2023 in Koivuniemi, Virolahti, Kymenlaakso. However, the measurement was made at ground level, so it could not be accepted as a record.

Wind

The most common wind direction in Finland is from southwest, but the low pressure areas typical for these latitudes cause great variations in wind speed and direction.

Storm, defined as at least one Finnish coastal station reporting at least 21 m/s as a 10-minutes average wind speed, is observed on Finnish seas on average 19 days a year. Strong winds are most frequent between October and January.

Snow

The first snow cover is observed on average in September in Lapland, and in November in Southern and western areas. Permanent snow cover time starts typically around Christmas in the Southwestern corner, but before mid-November in most of Lapland. The maximum snow depth is usually found around March.

Snow and supercooled droplets can accumulate in tree crowns and cause damage to trees. The trunks of pine trees can break under the weight of a snow-loaded crown, and deciduous trees can bend permanently. The snow load of a tree is typically 100–150 kg per one meter tree trunk, but the heaviest measured snow load of a spruce was over 3000 kilograms.

Snowmelt contributes to spring floods. In north, the peak flow of rivers always happens in spring, in the south 70–80% of floods happen in spring. In the south, maximum flow happens in mid-April, in the north, in mid-May.

It is predicted that as the Barents Sea gets less frozen in the coming winters and it becomes thus "Atlantified" additional evaporation will increase future snowfalls in Finland and much of continental Europe.