1) meridional wind anomaly
经向风异常
1.
,occurring in spring,developing in summer,maturing in autumn and decaying in winter,meanwhile,the meridional wind anomaly and its divergence both are closely related.
利用1982~1999期间LDEO海表温度资料和NCEP/NCAR再分析风场资料,分析东太平洋暖池及经向风异常与ENSO事件的可能关系。
2) zonal wind anomaly
纬向风异常
3) anomalous zonal wind
异常纬向风
1.
Actually, the anomalous zonal wind at the equatorial western Pacific is the main force to push the anomalies of subsurface ocean temperature in the war.
然而 ,赤道西太平洋异常纬向风是造成次表层海温异常东传的重要原因 ,而纬向风的异常又是由于东亚冬季风异常活动所引起的 ,这间接地说明了异常东亚冬季风对西太平洋暖池次表层海温距平东传的重要作用。
4) zonal wind anomalies in high and low troposphere
高低层纬向风异常
5) coastal low
异常风浪
1.
The fiercely developed coastal low that appears frequently along the South African coast often brings about abnormal weather.
通过对这种异常风浪的分析,结合船舶气象导航的具体工作列举了一个具体的个例,给出船舶经过该海域时应以避让为主,密切注意周围站点的气压场和风场的变化,一旦遇到恶劣的天气和海况时应根据具体情况选择最佳的避风场所。
6) westerly anomalies
西风异常
1.
Based on NCEP/NCAR reanalysis data and the trade wind indices provided by the Climate Prediction Center,it is revealed that during the onset and development phase of ENSO,the equatorial western Pacific westerly anomalies(WPWA) prevail during March-April-May(MAM) and August-September-October(ASO),respectively.
根据NCEP/NCAR再分析资料和美国气候预测中心提供的赤道太平洋信风指数,发现在ENSO年3~5月(MAM)和8~10月(ASO),赤道西太平洋存在两次显著的西风异常盛行期,并分析了这两次西风异常长时间维持的原因。
2.
The results have shown that the trend of upper oceanic heat storage(0~400m) and the westerly anomalies are well consistent with those on the tropical activity.
分析结果发现在西北太平洋海域,热带气旋活动趋势与上层海洋热力异常变化(上层海洋热含量)以及对流层低层的西风异常之间有着显著的相关关系,而与海洋表面温度无显著关系。
补充资料：靡然向风
1.亦作"靡然乡风"。亦作"靡然向风"。 2.谓群起效尤而成风气。
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