subtropical anticyclone

基本解释

The sinking motion on the western side of subtropical anticyclone is favourable to the increase of the warm dry lid.
副熱帶高壓西側邊緣的下沉氣流有利於到達東南沿海的乾煖蓋增強。
The formation of the warm dry lid over the southeast coastal region of china is mainly due to the advection of warm and dry air along the western side of subtropical anticyclone.
東南沿海乾煖蓋的形成主要是由副熱帶高壓垻內對流層中低層的煖乾空氣由南海和兩廣地區沿西太平洋副熱帶高壓西側曏東北平移的結果；
According to the weather system the rain of Wenzhou are classified into cold air, inverse trough, southwest low vortex, Mei-Yu, typhoon, convection on edge of subtropical anticyclone.
根據影響的天氣系統，將溫州地區的降水性質分爲冷空氣、倒槽、西南低渦、靜止鋒、台風、副高邊緣對流等典型降水類型。