Solar radiation has a lower intensity in polar regions because the angle at which it hits the earth is not as direct as at the equator. Another effect is that sunlight has to go through more atmosphere to reach the ground.[1]
Thepolar climate regions are characterized by a lack of warmsummers but with varyingwinters. Every month a polar climate has an average temperature of less than 10 °C (50 °F). Regions with a polar climate cover more than 20% of the Earth's area. Most of these regions are far from theequator and near thepoles, and in this case, winter days are extremely short and summer days are extremely long (they could last for the entirety of each season or longer). A polar climate consists of cool summers and very cold winters (or, in the case of ice cap climates, no real summer at all), which results in treelesstundras,glaciers, or a permanent or semi-permanent layer ofice. It is identified with the letterE in theKöppen climate classification.
There are two types of polar climate:ET, ortundra climate; andEF, orice cap climate. A tundra climate is characterized by having at least one month whose average temperature is above 0 °C (32 °F), while an ice cap climate has no months averaging above 0 °C (32 °F).[2] In a tundra climate, evenconiferous trees cannot grow, but other specialized plants such as the arctic poppy can grow. In an ice cap climate, no plants can grow, and ice gradually accumulates until it flows or slides elsewhere. Manyhigh altitude locations on Earth have a climate where no month has an average temperature of 10 °C (50 °F) or higher, but as this is due to elevation, this climate is referred to asAlpine climate. Alpine climate can mimic either tundra or ice cap climate.
On Earth, the only continent where the ice cap polar climate is predominant isAntarctica. All but a few isolated coastal areas on the island ofGreenland also have the ice cap climate. Summits of many high mountains also have ice cap climate due to their high elevation. Coastal regions of Greenland that do not have permanent ice sheets have the less extreme tundra climates. The northernmost part of theEurasian land mass, from the extreme northeastern coast ofScandinavia and eastwards to theBering Strait, large areas of northernSiberia and northernIceland have tundra climate as well. Large areas in northernCanada and northernAlaska have tundra climate, changing to ice cap climate in the most northern parts of Canada. SouthernmostArgentina (Tierra del Fuego where it abuts theDrake Passage) and such subantarctic islands such as theSouth Shetland Islands and theFalkland Islands havetundra climates of slighttemperature range in which no month is as warm as 10 °C (50 °F). These subantarctic lowlands are found closer to theequator than the coastal tundras of the Arctic basin. Summits of many mountains ofEarth also have polar climates, due to their higher elevations.
A map of the Arctic. The red line indicates the 10°Cisotherm in July and the white area shows the average minimumextent of sea ice insummer as of 1975.[3]
Some parts of the Arctic are covered by ice (sea ice,glacial ice, orsnow) year-round, especially at the most poleward parts; and nearly all parts of the Arctic experience long periods with some form of ice or snow on the surface. 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.
The Arctic consists ofocean that is almost surrounded by landmasses likeRussia andCanada. As such, theclimate of much of theArctic is moderated by the ocean water, which can never have a temperature below −2 °C (28 °F). In winter, this relatively warm water, even though covered by thepolar ice pack, keeps theNorth Pole from being the coldest place in theNorthern Hemisphere, and it is also part of the reason thatAntarctica is so much colder than the Arctic. In summer, the presence of the nearby water keeps coastal areas from warming as much as they might otherwise, just as it does intemperate regions withmaritime climates.
There have been several attempts at quantifying what constitutes a polar climate.
ClimatologistWladimir Köppen demonstrated a relationship between the Arctic and Antarctic tree lines and the 10 °C (50 °F) summer isotherm; i.e., places where the average temperature in the warmest calendar month of the year is below the fixed threshold of 10 °C (50 °F) cannot support forests. SeeKöppen climate classification for more information.
Otto Nordenskjöld theorized that winter conditions also play a role: His formula isW = 9 − 0.1C, whereW is the average temperature in the warmest month andC the average of the coldest month, both in degrees Celsius. For example, if a particular location had an average temperature of −20 °C (−4 °F) in its coldest month, the warmest month would need to average 11 °C (52 °F) or higher for trees to be able to survive there as9 − 0.1(−20) = 11. Nordenskiöld's line tends to run to the north of Köppen's near the west coasts of the Northern Hemisphere continents, south of it in the interior sections, and at about the same latitude along the east coasts of both Asia and North America. In the Southern Hemisphere, all ofTierra del Fuego lies outside the polar region in Nordenskiöld's system, but part of the island (includingUshuaia,Argentina) is reckoned as being within the Antarctic under Köppen's.
In 1947,Holdridge improved on these schemes, by definingbiotemperature: the mean annual temperature, where all temperatures below 0 °C or 32 °F (and above 30 °C or 86 °F) are treated as 0 °C (because it makes no difference to plant life, being dormant). If the mean biotemperature is between 1.5 and 3 °C (34.7 and 37.4 °F),[5] Holdridge quantifies the climate assubpolar (or alpine, if the low temperature is caused by elevation).
