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1)  East Asia summer moonsoon enhancement
东亚夏季风增强
2)  East Asian summer monsoon intensity
东亚夏季风强度
3)  East Asia summer monsoon
东亚夏季风
1.
Wave-packet propagation feature of East Asia summer monsoon in 1998;
1998年东亚夏季风波包传播特征研究
2.
On the basis of analyzing the relationship between the setting of the East Asia summer monsoon over the South China Sea(the South China Sea monsoon) and the outbreak of harmful algal bloom over the East China Sea, the result of analyses shows that over three weeks after the South China Sea monsoon breaks out, the harmful algal bloom will occur over the East China Sea.
通过分析东亚夏季风在南海的爆发(南海夏季风)与东海赤潮之间的关系,发现南海夏季风爆发后的1~3周内,东海有一次赤潮过程。
3.
East Asia summer monsoon has a distinct interannual variability,and the external forcing is one of main causes resulting in the interannual difference of East Asia summer monsoon,but the effect of the tropical sea surface temperature is the most prominent.
4区的海温异常变化和高低空纬向风垂直切变之间的关系,发现海温异常变化与东亚夏季风的环流场之间也有很好的关系。
4)  East Asian summer monsoon
东亚夏季风
1.
Features of interdecadal changes of the East Asian summer monsoon and similarity and discrepancy in ERA-40 and NCEP/NCAR Reanalysis;
东亚夏季风年代际变化的若干重要特征及两份大气再分析资料的异同
2.
Recent progresses of studies on influence of ENSO on the East Asian summer monsoon and China summer rainfall;
ENSO对东亚夏季风和我国夏季降水的影响研究进展
3.
Abrupt Character of the East Asian Summer Monsoon Recorded in the Annual Layer Thickness of Stalagmites During the Last Deglaciation;
末次冰消期东亚夏季风突变性的石笋年纹层记录
5)  East-Asian summer monsoon
东亚夏季风
1.
A nonlinear projection of the East-Asian summer monsoon onto the summer precipitation over China was performed by applying a neural-network-based nonlinear canonical correlation analysis method(NLCCA).
运用一种基于人工神经网络的非线性典型相关分析方法(NLCCA),对中国夏季降水与东亚夏季风之间的非线性关系进行了分析。
6)  the East Asian summer monsoon
东亚夏季风
1.
,the South Asian summer monsoon(SASM) over area(0°-25°N,60°E-100°E) and the East Asian summer monsoon(EASM) over area(0°-45°N,100°E-140°E) in boreal summer,and the North Australian summer monsoon(NASM) over area(0°-15°S,110°E-150°E) in austral summer,are investigated by using the ERA-40 daily reanalysis data,the NCEP/NCAR daily reanalysis data and the Climate Predicti.
利用1979~2002年的ERA-40和NCEP/NCAR逐日再分析资料以及CMAP降水资料探讨了亚澳季风各夏季风子系统(南亚夏季风、东亚夏季风、北澳夏季风)水汽输送的气候学特征及其与夏季降水的关系。
2.
,the South Asian summer monsoon(SASM) over the area(0°-25°N,60°E-100°E) and the East Asian summer monsoon(EASM) over the area(0°-45°N,100°E-140°E) in boreal summer,and the North Australian summer monsoon(NASM) over the area(0°-15°S,110°E-150°E) in austral summer,are respectively investigated.
利用1979~2003年的NCEP/NCAR再分析资料探讨了亚澳季风各夏季风子系统(南亚夏季风、东亚夏季风、北澳夏季风)流场结构及其季节演变的气候学特征。
3.
The interannual and interdecadal variations of the northerly wind system circulating around the west side of the Tibetan Plateau and their relation to the East Asian summer monsoon and the summer rainfall in North China are analyzed from the observed data.
从观测资料分析了青藏高原西侧绕流偏北风系的年际和年代际变化及其与东亚夏季风和华北地区夏季降水的关系。
补充资料:"大东亚共荣圈"
      见太平洋战争。
  

说明:补充资料仅用于学习参考,请勿用于其它任何用途。
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