1) Continental warm high pressure
大陆暖高压
2) warm high-pressure of Qinghai-Tibet Continent
青藏大陆暖高
3) continental high
大陆高压
1.
Based on the analysis of the general circulation, sub-tropical system, Continental High, and South Asian high, it is concluded that the formation of the drought in 2002 over the Sichuan Basin was mainly caused by the Continental High which maintained for a long time, while the sub-tropical weather system was weaker than that in normal years.
通过对副热带系统、大陆高压、南亚高压等夏季主要环流系统进行分析得出 ,2 0 0 2年汛期期间四川盆地的高温干旱天气主要是由稳定维持的大陆高压所造成。
4) continental high atmospheric pressure
大陆高气压
5) Land sub tropical high pressure
大陆副热带高压
6) continental high pressure
大陆性高气压
补充资料：暖高压
暖高压
多出现在副热带地区，有时也会在中高纬度地区出现。若中心暖于四周的高压(反气旋)，系统深厚，垂直伸展范围很大，有时可达到平流层底部。
说明：补充资料仅用于学习参考，请勿用于其它任何用途。
参考词条