也称暖性反气旋。温度大于四周，范围随高度而增大，到某高度后达到最大的高压系统。它不同于冷高压，是一种深厚的天气系统，可以从对流层下层一直伸展到对流层项或更高的高度。
受地形影响，偏西风造成的焚风效应和高压后部偏南风造成的暖湿空气在山前积聚，分别加剧了两类高温的强度。
Affected by topography, they were strengthened by the foehn effect caused by west wind and the warm moisture accumulation before mountains caused by south wind.
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；
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.
文中研究了热带西太平洋暖池和西太平洋副热带高压的季节性变化和年际变化关系。
The relationship of seasonal variation and interannual change between tropical western Pacific warm pool and western Pacific subtropical high have been discussed.
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