1) 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
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) Asian monsoon
东亚季风
1.
Since the beginning of the Quaternary, with the uplift of Tibetan Plateau, the Asian monsoon was established and became the controlling factor of the climate and environmental change of China.
自第四纪以来,青藏高原的隆升以及因此而建立起来的东亚季风季风系统成为我国气候、环境的最主要控制因素。
2.
Since late Tertiary, with the rapid uplift of Qing-Zang plateau, the whole china mainland had experienced the dramatic topographical reversal, which results in a series of large change in paleo-environmental evolution, including the formation of eastern-directed flowing river system, initiation of Asian monsoon, transgression and regressi.
从此导致长江、黄河等东流水系发育，东亚边缘海形成，东亚季风盛行等一系列的亚洲乃至全球环境变化格局。
4) 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 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。
补充资料：东亚季风
盛行于东亚地区的季风。中国、朝鲜和日本都属于东亚季风区。
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