1) equatorial meridional wind
赤道经向风
2) tropical zonal wind
赤道纬向风
1.
The interannual variability of tropical zonal wind and the relationship between ENSO and the Asian/Australian monsoon in different phases are discussed.
结果表明:赤道纬向风变化与中东太平洋海温变化在准四年周期上是强烈耦合的;在El Nino期间东亚冬季风弱,夏季风强,而南亚夏季风弱,反之,在 La Nina期间东亚冬季风强,夏季风弱,而南亚夏季风强;东亚地区的异常北风有利于西太平洋西风异常爆发,使得东太平洋海温升高,但只有随后在中东太平洋出现持续性西风异常,El Nino才能发展,其中来自太平洋中部的异常北风(并不是来自东亚大陆地区)和南太平洋中部的异常南风的辐合对中东太平洋出现持续性西风异常起重要的作用,尤其是澳大利亚东北部的季风异常的影响更为显著。
3) equatorial zonal wind
赤道纬向风场
4) equatorial westernes
赤道西风
5) cross equatorial meridional overturning circulation
越赤道经向翻转环流
1.
The interannual variability of the cross equatorial meridional overturning circulation in January(winter) and July(summer) for the Indian Ocean is studied based on the SODA data covering 50 years.
利用50 a的SODA资料对1月(冬季)和7月(夏季)印度洋越赤道经向翻转环流的年际变化进行研究。
6) equatorial westerly
赤道西风带
1.
Having analyzed the ECMWF wind data of recent years, this paper found that the establishment of Summer monsoon over the South China Sea occurs around the middle of May, which is characterized by northeastward stretching of the equatorial westerly belt and forming of an east-west-oriented flow shear along the coast of South China.
分析近年欧洲中心５月份逐日格点风资料，发现南海季风建立在５月中旬，其流场特征为赤道西风带向东北伸展，并汇入华南沿海的横向切变线内。
补充资料：向风
仰慕的意思：天下学士，靡然向风。
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