1) Paleo-winter monsoon
古冬季季风
2) winter and summer palaeo-monsoon
冬夏古季风
3) Winter monsoon
冬季季风
1.
The results show that(1)the YSWC strength obviously has an interannul variation of 4~7 years period,being well corretated to the longitudinal component of winter monsoon,(2)the YSWC path has a 3～7 years period,obviously influenced by the latitudinal component of winter monsoon,and(3)when the winter monsoon strenthens,YSWC becomes stronger and its path shifts westward.
利用了多年连续的冬季水文调查数据,以黄海暖水舌作为黄海暖流的示性指标,采用经验函数正交分解及相关分析的方法,探讨了黄海暖流的年际变化特征,结果表明:1)黄海暖流的强弱存在4～7a的年际变化周期,并与冬季局地季风的经向分量具有较好的相关关系;2)黄海暖流的流轴存在一个3～6a的变化周期,而且其流轴的摆动明显受冬季季风纬向分量的影响;3)季风增强,黄海暖流增强且流轴西移。
4) winter monsoon
冬季季节风
5) winter monsoon
冬季季(候)风
6) winter monsoon
冬季风
1.
Impact of ENSO Events on East Asian Winter Monsoon;
ENSO事件对东亚冬季风影响的研究
2.
Studies on loess sections through Loess Plateau in Central China suggested that >30 μm size fraction is a sensitive proxy of winter monsoon strength for central part of loess plateau.
通常把＞３０ μｍ颗粒含量作为冬季风的替代指标。
3.
The Modaomen estuarine circulation under a winter monsoon is discussed based on the synchronously surveyed data of spring tide and moderate tide during Dec.
通过理论分析和模型计算,表明向海的冬季风对河口垂向环流的形成起着重要的作用。
补充资料：季风(见季风气候)
季风(见季风气候)
j!feng候季风见季风气
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