1) subpolar westerlies
副极地西风带
2) polar westerlies
极地西风带
3) styrol subpolar region
副极地带
4) subtropical westerly jet
副热带西风急流
1.
Sensitive experiments were performed by using a regional climate model with p-σ incorporated coordinate to investigate the impacts of the uplift of the Tibetan Plateau on the East Asian subtropical westerly jet(EAWJ).
利用p-σ九层区域气候模式进行高原隆升对东亚副热带西风急流影响的敏感性试验,分析高原隆升过程中西风急流垂直结构和水平结构的变化,并对其变化的原因进行初步分析。
2.
They are (1) preparation stage of Subtropical westerly jet (from May to September); (2) Development stage of jet from October to March; (3) the jet disappearing and replacing by west pacific subtropical high from May to September.
我国夏季主雨带的形成 ,是从上一年夏季开始的 ,共经历 3个阶段 :①上一年 5～ 9月副热带西风急流的孕育期 ;② 10～ 3月西风急流发展期 ;③西风急流为西太平洋副热带高压替代期 (本年 5～ 9月 )———主雨带形成。
5) West Asia subtropical westerly jet stream
西亚副热带西风急流
6) subpolarlow-pressurebelt
副极地低压带
补充资料：副热带
亚热带。
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