3) westly jet
西风带急流轴
1.
Results are as follows:(1)The cold air and the shortwave trough disrupted from the westly jet at the level of 500 hPa which moved from the Ural Mountain to the Balkhash Lake,moved along the bottom of the jet to the Hexi Corridor of Gansu and the middle part of Qinghai,which provided energy for the ra.
利用Micaps常规和ECWMF资料,对造成2004年5月28～29日甘肃省中东部初夏区域性暴雨过程的高、低空急流及锋区等天气系统进行分析,结果表明:(1)500hPa西风带急流轴(≥20m。
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) high sky strong wind
高空副热带急流
1.
The result enunciation:In spring high sky strong wind is result in southeast region in Yunnan of one of the important factors of the unsteady la yer knot of atmosphere, the weather system tr.
结果表明,春季高空副热带急流是造成滇东南地区大气不稳定层结的重要因子之一,天气系统触发不稳定大气层结产生强冰雹云,副热带急流具有加强、维持发展的作用。
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