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‘eye’ of storm
‘eye’ of storm The central part of a tropical cyclone, where winds are light, skies are generally clear, and there is a slight, horizontal pressure gradient. The diameter of the ‘eye’ averages 20 km but in a large cyclone can be 40 km or more. The ‘eye’ is an area of some air subsidence which produces adiabatic warming.
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Cite this article
MICHAEL ALLABY. "‘eye’ of storm." A Dictionary of Ecology. 2004. Encyclopedia.com. 31 May. 2012 <http://www.encyclopedia.com>. MICHAEL ALLABY. "‘eye’ of storm." A Dictionary of Ecology. 2004. Encyclopedia.com. (May 31, 2012). http://www.encyclopedia.com/doc/1O14-eyeofstorm.html MICHAEL ALLABY. "‘eye’ of storm." A Dictionary of Ecology. 2004. Retrieved May 31, 2012 from Encyclopedia.com: http://www.encyclopedia.com/doc/1O14-eyeofstorm.html |
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‘eye’ of storm
‘eye’ of storm Central part of a tropical cyclone with light winds, generally clear skies, and a slight, horizontal pressure gradient. The diameter of the ‘eye’ averages 20 km but in a large cyclone can be 40 km or more. The ‘eye’ is an area of some air subsidence which produces adiabatic warming.
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Cite this article
AILSA ALLABY and MICHAEL ALLABY. "‘eye’ of storm." A Dictionary of Earth Sciences. 1999. Encyclopedia.com. 31 May. 2012 <http://www.encyclopedia.com>. AILSA ALLABY and MICHAEL ALLABY. "‘eye’ of storm." A Dictionary of Earth Sciences. 1999. Encyclopedia.com. (May 31, 2012). http://www.encyclopedia.com/doc/1O13-eyeofstorm.html AILSA ALLABY and MICHAEL ALLABY. "‘eye’ of storm." A Dictionary of Earth Sciences. 1999. Retrieved May 31, 2012 from Encyclopedia.com: http://www.encyclopedia.com/doc/1O13-eyeofstorm.html |
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