Subarctic climate

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Regions having a subarctic climate (also called boreal climate) are characterized by long, usually very cold winters, and brief, warm summers. It is found on large landmasses, away from the moderating effects of an ocean, generally at latitudes from 50° to 70°N. No such places exist in the Southern Hemisphere, so this climate does not exist outside the Northern Hemisphere. These climates represent Koppen climate classification Dfc, Dwc, Dfd and Dwd.

This type of climate offers some of the most extreme seasonal temperature variations found on the planet: In winter, temperatures can drop to −40 ℃ (−40 ℉) and in summer, the temperature may exceed +30 ℃ (86 ℉). However, the summers are short; no more than three months of the year (but at least one month) and must have a 24-hour average temperature of at least +10 ℃ (50 ℉) to fall into this category of climate. The subarctic climate is a subset of the continental climate. The subarctic climate is found in the following areas:

With 5-7 consecutive months where the average temperature is below freezing, all moisture in the soil and subsoil freezes solidly to depths of many feet. Summer warmth is insufficient to thaw more than a few surface feet, so permafrost prevails under large areas. Seasonal thaw penetrates from 2 to 14 ft (0.6 to 4 m), depending on latitude, aspect, and type of ground.[1] Some northern areas with subarctic climates located near oceans (southern Alaska and the northern fringe of Europe), have milder winters and no permafrost, and are thus more suited for farming.

The frost-free season is very short, varying from about 45 to 100 days at most, and a freeze can occur during any month in many areas. Vegetation in a subarctic climate is generally of low diversity, as only hardy species can survive the long winters and make use of the short summers. Trees are mostly limited to ferns and evergreen conifers, as few broadleaved trees are able to survive the very low temperatures in winter. This type of forest is also known as taiga, a term which is sometimes applied to the climate found therein as well. Even though the diversity may be low, numbers are high, and the taiga (boreal) forest is the largest forest biome on the planet, with most of the forests located in Russia and Canada.

Agricultural potential is generally poor, due to the natural infertility of soils and the prevalence of swamps and lakes left by departing ice sheets, and short growing seasons prohibit all but the hardiest of crops. (Despite the short season, the long summer days at such latitudes do permit some agriculture.) In some areas, ice has scoured rock surfaces bare, entirely stripping off the overburden. Elsewhere rock basins have been formed and stream courses dammed, creating countless lakes. [1]

There is very little precipitation, no more than 15 inches (38 cm) over an entire year and, away from the coasts, occurs mostly in the warmer months. Low precipitation, by the standards of more temperate regions with longer and warmer winters, is typically sufficient in view of the very low evapotranspiration to allow a water-sogged terrain in many areas of subarctic climate.

Should one go poleward or even toward a polar sea, one finds that the warmest month has an average temperature of less than 10°C (50°F), and the subarctic climate grades into a tundra climate even less suitable for trees.

Sample locations with such climates[2]:

Sample locations with the extreme Dfd climate include:

[edit] References

  1. ^ a b Subarctic Division
  2. ^ Subarctic Climate
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Climate types under the Köppen climate classification
Class A
Class B
Class C
Class D
Class E
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