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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 .
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.
Download as PDF; Printable version; In other projects ... Pages in category "Trees of subpolar oceanic climate" ... Text is available under the Creative Commons ...
Regions where oceanic or subtropical highland climates (Cfb, Cfc, Cwb, Cwc) are found. An oceanic climate, also known as a marine climate or maritime climate, is the temperate climate sub-type in Köppen classification represented as Cfb, typical of west coasts in higher middle latitudes of continents, generally featuring cool to warm summers and cool to mild winters (for their latitude), with ...
The polar circles are imaginary lines shown on maps to be the areas that receives less sunlight due to less radiation. These areas either receive sunlight (midnight sun) or shade (polar night) 24 hours a day because of the earth's tilt. Plants and animals in the polar regions are able to withstand living in harsh weather conditions but are ...
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Rawat Fault line near Islamabad. The geology of Pakistan encompasses the varied landscapes that make up the land constituting modern-day Pakistan, which are a blend of its geological history, and its climate over the past few million years. The Geological Survey of Pakistan is the premier agency responsible for studying the country's geology. [1]
The red line indicates the 10°C isotherm in July and the white area shows the average minimum extent of sea ice in summer as of 1975. [ 3 ] Some parts of the Arctic are covered by ice ( sea ice , glacial ice , or snow ) year-round, especially at the most poleward parts; and nearly all parts of the Arctic experience long periods with some form ...