Concept information
Preferred term
空气流动
Definition
- 地球大气循环中的空气流动，也叫行星风。主要由两个力分量引起：第一，纬度子午线上的力分量即地球自转偏向力（由G.G. de Coriolis在1835年提出的一种偏向运动或偏向力：地球的自传导致横越其表面的物体移动在北半球的时候向右偏转，在南半球向左偏转）；第二，经度纵向分量和垂直运动，主要由地球表面温度差分加热和冷却造成的不同压力分布所引起。
Broader concept
Belongs to group
Belongs to array
- ATMOSPHERE (air, climate) (en)
- gemet:groupCollection (gemet)
- gemet:superGroupCollection (gemet)
- NATURAL ENVIRONMENT, ANTHROPIC ENVIRONMENT (en)
In other languages
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Arabic
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Armenian
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Azerbaijani
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Basque
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Bulgarian
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Catalan
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Croatian
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Czech
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Danish
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Dutch
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English
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Estonian
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Finnish
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ilmakuljetus
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French
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Georgian
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German
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Greek
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Hungarian
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Icelandic
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Irish
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Italian
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Latvian
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Lithuanian
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Maltese
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Norwegian
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Polish
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Portuguese
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Romanian
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Russian
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Slovak
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Slovenian
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Spanish
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Swedish
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förflyttning av luftmassor
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Turkish
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Ukrainian
URI
http://www.eionet.europa.eu/gemet/concept/262
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