在南半球，反气旋绕高压中心反时针方向吹，与北半球情况相反。
In the Southern Hemisphere an anticyclone circulates counterclockwise around the high-pressure center, as contrasted to the Northern Hemisphere.
第二种是反气旋，当围绕高压中心形成风系统时出现反气旋。
Second is anticyclone this happens when winds form a wind system around a high.
例如375毫巴上单纯非地转风的流场的反气旋涡旋，适应后可建立起对流层暖性、平流层是冷性的高压系统。
For example, a non-geostrophic vortex in wind field on the 375 MB level can result in a high with the warm center in the troposphere and the cold center in the stratosphere.
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