At that time , there was an extensive rainband over the east china sea and the southeastern part of china . this rainband had the effect of washing out any dust moving southward 与此同时，一道广阔雨带正覆盖著东海及中国东南部，这道雨带能有效地冲刷掉任何南移的沙尘。
At that time , there was an extensive rainband over the east china sea and the southeastern part of china . this rainband had the effect of washing out any dust moving southward 与此同时，一道广阔雨带正覆盖著东海及中国东南部，这道雨带能有效地冲刷掉任何南移的沙尘。
The variation in the early aao beget the rainband latitudinal discrepance of the china summer monsoon by means of impacting on the intensity and position of northwest pacific subtropical high in the late summer 前期aao偏强时，后期6 ? 7月长江流域降水将增加，反之亦然。前期aao的变化通过影响后期夏季西北太平洋副高的强度和位置，引起中国夏季风雨带位置的南北偏差。
And the precipitation modes " characteristic of stations is the same as the representative variety during the meiyu : mostly centralized along the coast , and affecting by the subtropical high , the rainband moves west and north in late of meiyu 6 )发现了影响梅雨的最主要的遥相关型( eap 、 eu和wp ) ，代表站点的降水模态特点也与梅雨的典型的分布相同：主要降水集中在沿海，受副高影响，梅雨后期雨带西伸北抬。
