1) retreat of monsoon
季风后退
2) season of the retreat of the monsoon
季风撤退季
3) backweathering
后退风化
4) summer monsoon set-up and retreat
夏季风的建立和撤退
6) 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。
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