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.
副热带高压西侧边缘的下沉气流有利于到达东南沿海的干暖盖增强。
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.
东南沿海干暖盖的形成主要是由副热带高压坝内对流层中低层的暖干空气由南海和两广地区沿西太平洋副热带高压西侧向东北平移的结果；
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.
根据影响的天气系统，将温州地区的降水性质分为冷空气、倒槽、西南低涡、静止锋、台风、副高边缘对流等典型降水类型。