在沿城市的垂直剖面流场上组成了闭合的局地环流圈，白天垂直上升运动明显。
The vertical flow over the urban generally consists of a close circulation characterized by strong daytime updrafts at the center city.
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.
可作垂直上升、下降、直线、旋转上升、曲线等各种运动。
The utility model can do various spots of vertical rise, fall, straight line, rotary rise, curve, etc.
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