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1)  East Asian monsoon region
东亚季风区
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)  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。
5)  effect on East Asian monsoon region
对东亚季风区的影响
6)  The northwest influence region of East Asian summer monsoon
东亚夏季风西北影响区
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。
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