1) Asia-Australia monsoon
亚奥季风
2) East Asia monsoon
东亚季风
1.
The results of monitoring the ecological transect in East Asia monsoon region by normalized difference vegetation index (NDVI) indicated the presence of a close relationship between the NDVI of each ecological belt and the advance and retreat of the East Asia monsoon.
用极轨气象卫星的归一化植被指数(NDVI)对中国东亚季风区的生态过渡带(样带)进行遥感监测研究。
2.
Also compared the simulation results for high and low air levels with NCEP re-analysis data to check the simulation ability of REMO for East Asia monsoon.
将欧洲区域气候模式REMO首次应用于东亚区域, 利用该模式对 1980 年和 1990 年东亚季风季节变化进行了模拟研究, 并将模拟结果与NCEP再分析资料进行比较, 以检验该模式对东亚季风的模拟能力。
3.
In 1993, the East Asia monsoon is weak and its onset is late, the precipitation of Qinghai-Xizang Plateau mainly o.
用小波分析方法研究了1993年和1994年青藏高原雨季降水的多时间尺度变化特征,结果表明,小波变换对高原上降水从活跃期到中断期之间突变的时间有很好的分辨能力,并发现强弱季风年高原降水的变化特征有很大的差异:即高原降水除了其季节变化外,强东亚季风年(1994年)还有明显的30～60天低频变化;弱东亚季风年(1993年)却是准双周的变化明显。
3) East Asian Monsoon
东亚季风
1.
Exploring High-Resolution Records of the Holocene East Asian Monsoon from Mud Sediments on Shelves of China Marginal Seas;
从陆架泥质沉积中寻找高分辨率的全新世东亚季风记录
2.
Sedimentary Characteristic of Terrigenous Clast of Site MD05-2905 in the Northeastern Part of South China Sea after 36ka and Evolution of East Asian Monsoon;
南海东北部MD05-2905站36ka BP以来的陆源碎屑沉积特征与东亚季风的演化
3.
Dominant empirical mode of wind fields over east Asian monsoon region anomaly and its connection with ENSO;
东亚季风区风场异常主要经验模态及其与ENSO的联系
4) South Asia monsoon
南亚季风
1.
Dynamic and numerical methods are used to study/discuss the mechanism of terrain/thermal effect and the production/maintenance of South Asia monsoon.
用动力分析和数值试验方法研究讨论了地形和热力效应与南亚季风产生和维持的动力机理。
2.
Furthermore,tree-ring δ18O shows negative and significant correlations with South Asia monsoon index and East Asia monsoon index in different periods.
同时,树轮δ18O年际变化与南亚季风指数、东亚夏季风指数呈反相关关系,并与1-5月南方涛动指数负相关显著,在一定程度上反映了大尺度的大气环流影响。
5) Asian summer monsoon
亚洲季风
1.
The relationship between the location change of the East Asian subtropical westerly jet(EASWJ) and Asian summer monsoon onset is investigated by using NCEP/NCAR pentad mean reanalysis data.
利用1961～2000年的NCEP/NCAR候平均再分析资料,初步探讨了季节转换期间东亚副热带西风急流南北和东西向位置变化与亚洲季风爆发之间的联系。
2.
By use of IAP9 AGCMⅡ, a numerical experiment is made, in which the influence of the south west Indian Ocean SSTA on the outbreak of the Asian summer monsoon has been discussed.
试验结果表明 ,当该海域 1～ 3月份的海温出现异常增暖时 ,印度夏季风和东亚夏季风的爆发均较平常晚 ,反之 ,二者的建立均较平常早 ;该海域 1～ 3月份的海温异常对亚洲季风区的降水也有明显的影
6) Asian monsoon
亚洲季风
1.
The spatial and temporal distribution features of onset period of mean rainy season over Asian monsoon region;
亚洲季风区平均雨季起始期的时空分布特征
2.
The variations of Asian monsoon as revealed by the variations of kinetic energy of barotropic/baroclinic modes of the wind field;
亚洲季风变动与大气正压/斜压运动动能变化的气候特征
3.
Thrusts and prospects on understanding and predicting Asian monsoon climate.;
认识和预报亚洲季风气候:前沿突破点和展望
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