暖高压

nuǎn gāo yā

暖高压

暖高压[nuǎn gāo yā]

1

在平流层中，北半球冬季为一较大的环极冷低压，夏季为一以整个半球为规模的环极暖高压。

In the stratosphere of Northern Hemisphere , there is a circumpolar cold low in winter , and for a circumpolar warm high in summer .
2

大陆深厚暖高压是造成高温干旱的主要天气系统。

Deep continental warm high is the primary reason of the hot and dry weather .
3

结果表明：在中高层暖性高压脊及地面变性冷高压稳定维持的大尺度背景条件下，地表净辐射引起的近地层冷却是大雾过程的触发和加强机制；

The results show that a warm high ridge at the middle level and transformed surface cold high over the plain provide a good background condition ; a cooling process produced by net surface radiation fluxes is the trigger and strengthening mechanism for the fog event ;