Search results
Results From The WOW.Com Content Network
The subarctic climate (also called subpolar climate, or boreal climate) is a continental climate with long, cold (often very cold) winters, and short, warm to cool summers. It is found on large landmasses, often away from the moderating effects of an ocean, generally at latitudes from 50°N to 70°N, poleward of the humid continental climates .
From Wikipedia, the free encyclopedia. Redirect page
The term sometimes denotes the form of climate characteristic of the zone of hemiboreal forests—specifically, the climates designated Dfb, Dwb and Dsb in the Köppen climate classification scheme. On occasion, it is applied to all areas that have long, cold winters and warm (but not hot) summers—which also including areas that are semiarid ...
This represents subarctic and subpolar oceanic climate realms, defined the same as in Köppen's scheme, where 1 to 3 months have an average temperature of 10 °C (50 °F) or above. In this climate zone there is only a short period (normally 50 to 90 days) that is frost free.
This page was last edited on 19 September 2020, at 19:56 (UTC).; Text is available under the Creative Commons Attribution-ShareAlike 4.0 License; additional terms may apply.
The Magellanic subpolar forests (Spanish: Bosque Subpolar Magallánico) are a terrestrial ecoregion of southernmost South America, covering parts of southern Chile and Argentina, [2] and are part of the Neotropical realm. It is a temperate broadleaf and mixed forests ecoregion, and contains the world's southernmost forests.
Climates are classified based on specific criteria unique to each climate type. [1] The Köppen climate classification is the most widely used climate classification scheme. [2] It was first published by German-Russian climatologist Wladimir Köppen (1846–1940) in 1884, [3] [4] with several later modifications by Köppen, notably in 1918 and ...
A Subpolar subhumid temperate climate, officially classified as a Cold subtropical highland climate or Monsoon-influenced subpolar oceanic climate under the Köppen classification (Cwc), is a sub-alpine climate. It is located only in Andean high plains in Bolivia and Perú, [2] from 3200 m until 4000 m.