subtropical anticyclone

基本解釋

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(cè)邊緣的下沉氣流有利於到達(dá)東南沿海的乾煖蓋增強(qiáng)。
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(nèi)對流層中低層的煖乾空氣由南海和兩廣地區(qū)沿西太平洋副熱帶高壓西側(cè)曏東北平移的結(jié)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(jù)影響的天氣系統(tǒng)，將溫州地區(qū)的降水性質(zhì)分爲(wèi)冷空氣、倒槽、西南低渦、靜止鋒、臺風(fēng)、副高邊緣對流等典型降水類型。