…In this state, the strong westerly wind component is in the southwesterly wind area, and the weak westerly wind component is in the northerly wind area, so u (westerly wind component) × v (southern wind component) becomes a very large value when viewed globally. If we consider the high and low pressure systems as one large eddy, momentum is transported from the equator to the mid-latitudes by such eddies, and this is called eddy transport. The mean meridional circulation transport and eddy transport work together to move angular momentum and heat to the poles, with the former predominating in the tropics and the latter in mid- and high-latitudes. … *Some of the terminology that refers to "eddy transport" is listed below. Source | Heibonsha World Encyclopedia 2nd Edition | Information |
…このような状態のときは強い西風成分が南西風の所にあり,弱い西風成分が北風成分の所にあるので,u(西風成分)×v(南風成分)は地球全体でみると非常に大きな値になる。高・低気圧を一つの大きな渦と考えると,このような渦によって運動量が赤道から中緯度に輸送されていることになり,これを渦輸送と呼ぶ。平均子午面循環輸送と渦輸送がいっしょになって,角運動量と熱を極に移動させており,熱帯地方では前者が卓越し,中・高緯度では後者が卓越する。… ※「渦輸送」について言及している用語解説の一部を掲載しています。 出典|株式会社平凡社世界大百科事典 第2版について | 情報 |
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