Climate of the Faroe Islands
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Faroe Islands The Faroe Islands ( ), or simply the Faroes ( fo, Føroyar ; da, Færøerne ), are a North Atlantic island group and an autonomous territory of the Kingdom of Denmark. They are located north-northwest of Scotland, and about halfway bet ...
are an island group consisting of eighteen islands between the
Norwegian Sea The Norwegian Sea ( no, Norskehavet; is, Noregshaf; fo, Norskahavið) is a marginal sea, grouped with either the Atlantic Ocean or the Arctic Ocean, northwest of Norway between the North Sea and the Greenland Sea, adjoining the Barents Sea to ...
and the North Atlantic, about half-way between
Iceland Iceland ( is, Ísland; ) is a Nordic island country in the North Atlantic Ocean and in the Arctic Ocean. Iceland is the most sparsely populated country in Europe. Iceland's capital and largest city is Reykjavík, which (along with its s ...
and
Norway Norway, officially the Kingdom of Norway, is a Nordic country in Northern Europe, the mainland territory of which comprises the western and northernmost portion of the Scandinavian Peninsula. The remote Arctic island of Jan Mayen and the ...
. Its coordinates are . It is 1,393 square kilometres in area, and includes small lakes and rivers, but no major ones. There are 1,117 kilometres of coastline, and no land boundaries with any other country. The Faroe Islands generally have cool summers and mild winters, with a usually overcast sky and frequent fog and strong winds. Although at a high latitude, due to the Gulf Stream their climate is ameliorated. The islands are rugged and rocky with some low peaks; the coasts are mostly bordered by cliffs. The Faroe Islands are notable for having the highest sea cliffs in Europe, and some of the highest in the world otherwise. The lowest point is at sea level, and the highest is at
Slættaratindur Slættaratindur (English: ''Flat peak'') is the highest mountain in the Faroe Islands, at an elevation of 880 metres. It is located in the northern part of Eysturoy, between the villages of Eiði, Gjógv, and Funningur. Funningur lies at the fo ...
, which is 882 metres above sea level. The landscape made roadbuilding difficult, and only recently has this been remedied by building tunnels. Many of the Faroese islands tend to be elongated in shape.
Natural resource Natural resources are resources that are drawn from nature and used with few modifications. This includes the sources of valued characteristics such as commercial and industrial use, aesthetic value, scientific interest and cultural value. ...
s include
fish Fish are aquatic, craniate, gill-bearing animals that lack limbs with digits. Included in this definition are the living hagfish, lampreys, and cartilaginous and bony fish as well as various extinct related groups. Approximately 95% of ...
and
hydropower Hydropower (from el, ὕδωρ, "water"), also known as water power, is the use of falling or fast-running water to produce electricity or to power machines. This is achieved by converting the gravitational potential or kinetic energy of a w ...
.


Statistics

;
Geographic coordinates The geographic coordinate system (GCS) is a spherical or ellipsoidal coordinate system for measuring and communicating positions directly on the Earth as latitude and longitude. It is the simplest, oldest and most widely used of the various ...
: :* :* North: Enniberg, 62°29′,2 N :* South: Sumbiarsteinur, 61°21′,6 N :* West: Gáadrangur, 7°40′,1 W :* East: Stapin, 6°21′,5 W ; Area: :* Land: 1,393 km² :* Water: 7.19 km² (the area includes 10 of the largest lakes. There are a number of smaller lakes and streams.) ; Land boundaries: : 0 km ; Coastline: : 1,117 km ; Maritime claims: :* Territorial sea: :* Continental shelf: or agreed boundaries or median line :* Exclusive economic zone: or agreed boundaries or median line ; Climate: : Subarctic oceanic climate (
Köppen climate classification The Köppen climate classification is one of the most widely used climate classification systems. It was first published by German-Russian climatologist Wladimir Köppen (1846–1940) in 1884, with several later modifications by Köppen, notabl ...
''Cfc'') moderated by
North Atlantic Current The North Atlantic Current (NAC), also known as North Atlantic Drift and North Atlantic Sea Movement, is a powerful warm western boundary current within the Atlantic Ocean that extends the Gulf Stream northeastward. The NAC originates from where ...
; long, mild, windy winters; short, cool summers, damp in the South and West. Arctic climate (Köppen ''ET'') in some mountains. ; Terrain: : Rugged, rocky, some low peaks; cliffs along most of coast. The coasts are deeply indented with
fjord In physical geography, a fjord or fiord () is a long, narrow inlet with steep sides or cliffs, created by a glacier. Fjords exist on the coasts of Alaska, Antarctica, British Columbia, Chile, Denmark, Förden and East Jutland Fjorde, Germany, ...
s, and the narrow passages between islands are agitated by strong tidal currents. Multiple
sea stacks A stack or sea stack is a geological landform consisting of a steep and often vertical column or columns of rock in the sea near a coast, formed by wave erosion. Stacks are formed over time by wind and water, processes of coastal geomorphology ...
exist along the coast. ; Elevation extremes: :* Lowest point: Atlantic Ocean 0 m :* Highest point:
Slættaratindur Slættaratindur (English: ''Flat peak'') is the highest mountain in the Faroe Islands, at an elevation of 880 metres. It is located in the northern part of Eysturoy, between the villages of Eiði, Gjógv, and Funningur. Funningur lies at the fo ...
880 m ; Natural resources: :
Fish Fish are aquatic, craniate, gill-bearing animals that lack limbs with digits. Included in this definition are the living hagfish, lampreys, and cartilaginous and bony fish as well as various extinct related groups. Approximately 95% of ...
,
whales Whales are a widely distributed and diverse group of fully aquatic placental marine mammals. As an informal and colloquial grouping, they correspond to large members of the infraorder Cetacea, i.e. all cetaceans apart from dolphins and ...
,
hydropower Hydropower (from el, ὕδωρ, "water"), also known as water power, is the use of falling or fast-running water to produce electricity or to power machines. This is achieved by converting the gravitational potential or kinetic energy of a w ...
,
wind Wind is the natural movement of air or other gases relative to a planet's surface. Winds occur on a range of scales, from thunderstorm flows lasting tens of minutes, to local breezes generated by heating of land surfaces and lasting a few ho ...
, possible
petroleum Petroleum, also known as crude oil, or simply oil, is a naturally occurring yellowish-black liquid mixture of mainly hydrocarbons, and is found in geological formations. The name ''petroleum'' covers both naturally occurring unprocessed crud ...
and
natural gas Natural gas (also called fossil gas or simply gas) is a naturally occurring mixture of gaseous hydrocarbons consisting primarily of methane in addition to various smaller amounts of other higher alkanes. Low levels of trace gases like carbo ...
; Land use: :* Arable land: 2.14% :* Permanent crops: 0% :* Other: 97.86% (2012) ; Environment—international agreements: : Marine dumping


Climate

The climate is classed as
subpolar oceanic climate An oceanic climate, also known as a marine climate, is the humid temperate climate sub-type in Köppen classification ''Cfb'', typical of west coasts in higher middle latitudes of continents, generally featuring cool summers and mild winters ...
(
Köppen climate classification The Köppen climate classification is one of the most widely used climate classification systems. It was first published by German-Russian climatologist Wladimir Köppen (1846–1940) in 1884, with several later modifications by Köppen, notabl ...
'' Cfc''), with areas having a
tundra In physical geography, tundra () is a type of biome where tree growth is hindered by frigid temperatures and short growing seasons. The term ''tundra'' comes through Russian (') from the Kildin Sámi word (') meaning "uplands", "treeless mou ...
climate, especially in the mountains, although some coastal or low-lying areas may have very mild-winter versions of a tundra climate. The overall character of the climate of the islands is influenced by the strong warming influence of the Atlantic Ocean, which produces the
North Atlantic Current The North Atlantic Current (NAC), also known as North Atlantic Drift and North Atlantic Sea Movement, is a powerful warm western boundary current within the Atlantic Ocean that extends the Gulf Stream northeastward. The NAC originates from where ...
. This, together with the remoteness of any source of landmass-induced warm or cold airflows, ensures that winters are mild (mean temperature 3.0 to 4.0 °C or 37 to 39 °F) while summers are cool (mean temperature 9.5 to 10.5 °C or 49 to 51 °F). The islands are windy, cloudy and cool throughout the year with an average of 210 rainy or snowy days per year. The islands lie in the path of depressions moving northeast, making strong winds and heavy rain possible at all times of the year. Sunny days are rare and overcast days are common.
Hurricane Faith Hurricane Faith was a long-lived Cape Verde hurricane and was the sixth named storm and fifth hurricane of the 1966 Atlantic hurricane season. Faith developed from an area of disturbed weather between Cape Verde and the west coast of Africa on A ...
struck the Faroe Islands on 5 September 1966 with sustained winds over 100 mph (160 km/h) and only then did the storm cease to be a tropical system.GHCN Climate data, Thorshavn series 1881 to 2007 Due to the altitude, ocean currents, topography, and winds, the islands exhibit a variety of
microclimate A microclimate (or micro-climate) is a local set of atmospheric conditions that differ from those in the surrounding areas, often with a slight difference but sometimes with a substantial one. The term may refer to areas as small as a few squ ...
s. Precipitation varies considerably throughout the archipelago. In some highland areas, snow cover may last for months with snowfalls possible for the greater part of the year (on the highest peaks, summer snowfall is by no means rare), while in some sheltered coastal locations, several years pass without any snowfall whatsoever. Tórshavn receives frosts more often than other areas just a short distance to the south. Snow is also seen at a much higher frequency than outlying islands nearby. The area receives on average 49 frosts a year. While receiving more frost than most of the Faroe Islands, Mykines is more temperate in the winter than nearby Vágar. Snow is also less common despite the relatively lower winter temperatures due to the relatively low precipitation in the area. It also has a very mild tundra climate bordering on subpolar oceanic. Frost occurs on 46 days in an average year It is also likely that the lower areas of the island experience less than this, as the weather station is located at 105 meters above sea level. Akraberg is milder than much of the Faroe Islands and experiences frost on 38 days in an average year, possibly less in lower areas, as the weather station is located at an elevation of 101 meters above sea level. Vágar has colder and snowier winters than most other places in the archipelago. Lower temperatures combined with higher precipitation are responsible for this, and measurable snow cover can be seen- a rarity in the Faroe Islands, in which snow cover (in areas which regularly experience it) is usually limited to a thin coating. The airport, at which data is recorded, is also located at a higher altitude on the island (84 meters above sea level), which might result in lower temperatures and higher precipitation than lower-lying areas on the island. Frost occurs on average on 62 days of the year, the most out of all stations included in the records of the Danish Meteorological Institute. Kirkja has a very mild climate, similar to Akraberg. It has the lowest frequency of frosts out of all weather stations included in the records by the Danish Meteorological Institute, with 36 days of frost in an average year. Snowfall is uncommon, due to mild temperatures and relatively low precipitation. The weather station is somewhat high at 53 meters above sea level, which could possibly affect the data, but not as much as the previous stations. Nólsoy experiences a climate that is quite typical of the surrounding area and the Faroe Islands in general, and is similar to nearby Tórshavn. There are on average 44 days of frost a year. Also, as in the case of previous weather stations, the location is higher on its respective island, and the climate of the lower areas of the island differs slightly. The climate of Sandur is typical for a low-lying coastal location in the south of the Faroe Islands, as the weather station for Sandur is located at 5 meters above sea level. On average, Sandur experiences 41 days of frost a year.


See also

*
List of islands of the Faroe Islands This is a list of islands of the Faroe Islands. There are 18 islands, of which Lítla Dímun is the only one uninhabited. Besides these 18 islands there are also several islets and skerries in the Faroes. See also *Geography of the Faroe Isl ...
* List of mountains of the Faroe Islands * Geology of the Faroe Islands * Extreme points of the Faroe Islands * Fjords in the Faroe Islands


Further reading

* Ostenfeld, C. H., and Eugenius Warming. ''Geography, Geology and Climate of the Faeröes, With the Historical Notes on the Botanical Investigation of These Islands''. Copenhagen: H.H. Thiele, 1901. * Peacock, Martin A. ''Recent Lines of Fracture in the Færoes in Relation to the Theories of Fiord Formation in Northern Basaltic Plateaux''. Glasgow: Jackson, Wylie, 1928.


References

* "Faroe Islands" ''World Fact Book 2004'', CIA, Washington. {{Geography of Europe