1) East-Asian winter/summer monsoon
东亚冬/夏季风
2) East Asian summer and winter monsoons
东亚冬夏季风
3) EastAsian winter and summer monsoon circulations
东亚冬、夏季风环流
4) East Asian Winter Monsoon
东亚冬季风
1.
Constructing a Recent 8 ka High-Resolution Record of East Asian Winter Monsoon from Sediments on Inner Shelf of East China Sea;
近8ka东亚冬季风记录在东海内陆架的建立
2.
The relationship between the spatial and temporal variation characteristics of the first mode(EOF1) of East Asian winter monsoon and climate change in China is revealed by using the vector EOF expansion of winter wind fields at 1 000 hPa over East Asia during 1951/1952～2003/2004.
结果表明,EOF1时间系数能够很好地刻画东亚冬季风的强度变化。
3.
Under this heterogeneous warming background,the sea-land thermal contrast would be changed and then may lead to the variation of East Asian winter monsoon(EAWM).
利用NCEP/NCAR再分析月平均海平面气压资料,定义了一个东亚冬季风强度指数(IWI),并发现20世纪60年代到70年代初期东亚冬季风强度减弱,其后冬季风强度有所增强,80年代初期以后东亚冬季风强度又开始减弱。
5) 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。
6) 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
补充资料：东亚
| 东亚 Eastern Asia 亚洲大陆的东部地区。通常指中国、蒙古、朝鲜、韩国和日本。东濒太平洋，边缘多群岛、半岛。面积约1170万平方千米，人口约14亿。位于亚洲大陆与太平洋海盆之间的过渡带上，地质构造复杂，地壳变动剧烈，多火山、地震。地势西高东低，山地丘陵为主，仅中国的东北、华北、华东有广阔的平原。大部属季风气候。大河多源于西部山地，向东流入太平洋。森林和水力资源丰富，矿藏种类多，储量大。沿海为世界著名渔场之一。产稻、小麦、大豆、棉花、麻、蚕丝、茶等。 |
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