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・ Polariffic
・ Polar body
・ Polar body biopsy
・ Polar Bowler
・ Polar Boy
・ Polar Capital Technology Trust
・ Polar capsule
・ Polar Caves Park
・ Polar cell
・ Polar Challenge
・ Polar circle
・ Polar circle (geometry)
・ Polar Circle Marathon
・ Polar city
・ Polar class
Polar climate
・ Polar Club Glacier
・ Polar code
・ Polar code (coding theory)
・ Polar code (maritime)
・ Polar concept argument
・ Polar Conservation Organisation
・ Polar coordinate system
・ Polar Cup
・ Polar curve
・ Polar curve (aerodynamics)
・ Polar decomposition
・ Polar desert
・ Polar diagram
・ Polar distance


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Polar climate : ウィキペディア英語版
Polar climate

Regions with a polar climate are characterized by a lack of warm summers. Every month in a polar climate has an average temperature of less than . Regions with polar climate cover over 20% of the Earth. The sun shines for long hours in the summer, and for many fewer hours in the winter. A polar climate results in treeless tundra, glaciers, or a permanent or semi-permanent layer of ice.
==Subtypes==

There are two types of polar climate: ET, or tundra climate; and EF, or ice cap climate. A tundra climate is characterized by having at least one month whose average temperature is above , while an ice cap climate has no months above . In a tundra climate, trees cannot grow, but other specialized plants can grow. In an ice cap climate, no plants can grow, and ice gradually accumulates until it flows elsewhere. Many high altitude locations on Earth have a climate where no month has an average temperature of or higher, but as this is due to elevation, this climate is referred to as Alpine climate. Alpine climate can mimic either tundra or ice cap climate.

抄文引用元・出典: フリー百科事典『 ウィキペディア(Wikipedia)
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