1) 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。
2) West Asia subtropical westerly jet stream
西亚副热带西风急流
3) subtropical westerlies jet in winter
冬季副热带西风急流
1.
Utilizing the radiosonde observation data during the 30 years(1961-1991),we calculate the vertical 16 layers distribution of subtropical westerlies jet in winter,and on the basis of the distribution model to regress the main pluvial regions year by year(according to two standards,i.
利用中国1961-1991年探空资料,分16层计算了冬季副热带西风急流的垂直分布,并用此分布模型"回套"1470-2006年共537年逐年夏季主雨带(按涝与不涝、旱与不旱两个标准),结果535年被"套中,"1778及1902年两年错误,成功率99。
4) 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。
6) 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