1) Asian-African summer monsoon
亚非夏季风
1.
Characteristics of Asian-African summer monsoon pre-and post-global warming in mid-1980s.;
20世纪80年代中期全球变暖前后亚非夏季风特征分析
2) 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。
3) 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
4) Asian summer monsoon
亚洲夏季风
1.
Interannual and interdecadal variations of moisture transport by Asian summer monsoon and their association with droughts or floods in China;
亚洲夏季风水汽输送的年际年代际变化与中国旱涝的关系
2.
Roles of tropical and subtropical land_sea distribution and the Qinghai-Xizang Plateau in the formation of the Asian summer monsoon;
热带、副热带海陆分布与青藏高原在亚洲夏季风形成中的作用
3.
The snow cover on the Tibetan Plateau has obvious seasonal,interannual and interdecadal changes,and is one of the most important factors which control the Asian summer monsoon precipitation.
青藏高原(以下简称高原)积雪具有明显的季节、年际和年代际变化特征,是影响亚洲夏季风降水的重要因子之一。
5) South Asian summer monsoon
南亚夏季风
1.
Using the observation data obtained in the Rongbuk Valley in June 2007 and the real-time NCEP/NCAR reanalysis data,the variation of surface wind and its possible responses to the South Asian summer monsoon(SASM) were analyzed.
利用2007年6月强化观测实验期间获得的大气观测资料和同时期的NCEP/NCAR大尺度再分析资料,结合2006年同期的分析结果,进一步研究了珠峰北坡绒布河谷地区的地面风场状况及其对南亚夏季风的响应,并与2006年的结果进行了比较。
2.
Qomolangma and its responses to the South Asian summer monsoon(SASM),using the observation data obtained during HEST2006 campaign in June 2006.
为了正确理解该环流系统与南亚天气气候过程的可能关联,本文利用HEST2006珠穆朗玛峰绒布河谷强化实验期间获得的2006年5~6月的地面观测资料和实时的大气环流资料,对该地区地面风场与南亚夏季风的关系进行了研究。
3.
The first mode of the deviation wind field shows the rapid changes of the South Asian summer monsoon circulation around the onset and time series reflect the onset of South Asian monsoon and the abrupt change of the atmos.
作者对南亚(印度)夏季风爆发作了统计动力分析,即将南亚夏季风爆发前后的高低层风场看作一个整体,并以南亚夏季风爆发日为基准,作了经验正交函数(矢量)分析,得到了以下结论:偏差风场的第一模态反映了季风爆发前后大规模的风系变化,其时间系数直接体现了南亚夏季风的爆发,在爆发日前后该模态反映的偏差风系有剧烈变化,这表明季风爆发时大气环流有突变发生;第二模态反映了具有5~7天振荡周期的中纬天气尺度波系及其对低纬季风区的影响;第三模态反映了热带、副热带地区呈准双周振荡的低频扰动。
6) 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。
补充资料：亚非
1.亚洲和非洲的并称。
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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