气旋环流，又称气旋式环流，是指在北半球（南半球）呈逆时针（顺时针）旋转流动的环流。例如低压系统（气旋、台风等）都是一种气旋式环流。
... cyclone track气旋路线 cyclonic circulation气旋环流 cyclonic flow气旋流动 ...
基于132个网页-相关网页
The western wind in low-level prevails in this region, and the vertical shear is weaken. The anomalous anti-cyclonic circulation are produced, hence the rainfall reduces over the region.
在中国南部地区高空为异常的偏西气流,意味着高空偏东风的减弱,而低层仍然为异常偏西风,该地区上空的垂直切变减弱,有利于反气旋环流的产生,因此导致东南沿海地区降水减少。
参考来源 - 青藏高原气候环境对冰川发育影响的数值模拟研究·2,447,543篇论文数据，部分数据来源于NoteExpress
结果该区域产生了垂直上升运动及负的涡度强迫源，对应着异常强烈的反气旋环流。
This generates ascent as well as negative vorticity source, which corresponds to a strongly anomaly anticyclone center appearing to the north of the heating region.
在异常的冬季风偏北风分量强迫下，西太平洋上形成的偏差气旋环流在夏季已不存在，这时东亚夏季风反而增强。
The northerly component of the winter monsoon anomaly makes the anomalous cyclone over the western Pacific not exist and the East Asian summer monsoon becomes stronger.
上新世早期的大气环流被减弱，因此垂直风切变减小，助长了热带气旋的发展。
Tthe early Pliocene had a weakened atmospheric circulation, and therefore, reduced vertical wind shear, which is favorable for tropical cyclone growth.
应用推荐