2) East Asia subtropical westerly jet
东亚副热带西风急流
1.
The monthly wind field of NCEP/NCAR reanalysis data is used to define an intensity index of the East Asia subtropical westerly jet, which can reasonably reflect the impact of the East Asia subtropical westerly jet on summer precipitation in North China.
利用NCEP/NCAR再分析资料,定义了一个东亚副热带西风急流强度指数,这个指数能够较好地反映东亚副热带西风急流强度变化对华北地区降水的影响。
3) 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。
4) tropical easterly flow
热带东风气流
1.
Then the depression formation in tropical easterly flow is discussed.
由此讨论了热带东风气流中的低压形成。
5) tropical easteries
热带东风带
6) southeast jet
东南风急流
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