副热带高压是指位于副热带地区的暖性高压系统。它对中、高纬度地区和低纬度地区之间的水汽、热量、能量的输送和平衡起着重要的作用，是夏季影响中国大陆天气的主要天气系统。
小笠原副热带高压 Ogasawara high
西太平洋副热带高压 West Pacific Subtropical High ; WPSH ; subtropical high over west pacific
副热带高压北跳与月尖 CUSP
副热带高压脊 subtropical ridge
副热带高压带 subtropical high belt ; subtropical high-pressure belt
副热带高压区 subtropical high pressure belt
夏季副热带高压 subtropical high in summer
对西太平洋副热带高压 West Paeific Subtropical high
副热带高气压 Sub-Tropical High
今年7月27日，受副热带高压，浙江仍在继续热浪。
In July 27th, by the subtropical high, Zhejiang is continuing heatwave.
而副热带高压的变化又会反过来影响降水区位置的变化。
Meanwhile, the changed subtropical high also affects the location of precipitation.
夏季，印度低压和东亚的季风低压均减弱；而副热带高压系统普遍增强。
Indian low and monsoon low of East Asia have the obvious weakness in summer and subtropical high system generally strengthens.
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