1) vertical circulation
季风垂直环流
2) monsoon
季风
1.
ZHENG He s Cognition And Utilization of Monsoon and Ocean Current During His Sailing;
郑和下西洋对季风洋流的认识和利用
2.
Process of monsoon variations of the northeastern Qinghai-Xizang Plateau from the loess record of Lonxi Basin since the last interglacial epoch;
陇西黄土沉积记录反映的末次间冰期以来青藏高原东北部季风的演化过程
3.
Some New Problems and New Methods in the Monsoon Study—An Introduction to the Special Issue;
前言——季风研究中的一些新问题和新方法
3) winter monsoon
冬季风
1.
Impact of ENSO Events on East Asian Winter Monsoon;
ENSO事件对东亚冬季风影响的研究
2.
Studies on loess sections through Loess Plateau in Central China suggested that >30 μm size fraction is a sensitive proxy of winter monsoon strength for central part of loess plateau.
通常把＞３０ μｍ颗粒含量作为冬季风的替代指标。
3.
The Modaomen estuarine circulation under a winter monsoon is discussed based on the synchronously surveyed data of spring tide and moderate tide during Dec.
通过理论分析和模型计算,表明向海的冬季风对河口垂向环流的形成起着重要的作用。
4) monsoon system
季风系统
5) monsoon climate
季风气候
1.
It is revealed that droughts often occur in the cold periods while floods in the warm,indicating the monsoon climate change.
结果显示本区气候总体冷期易旱、暖期易涝,显示季风气候区的特征。
2.
Seasonal variations of particulate matter and diatom fluxes in the northern South China Sea during 1987-1988 were overwhelmingly controlled by monsoon climate.
南海北部１９８７年９月～１９８８年１０月沉积物捕获器中颗粒物质和硅藻通量的季节性 变化受到季风气候的控制。
3.
The influence of the monsoon climate on the isotopic composition of precipitation is discussed based on the accumulated data in China.
根据我国积累的雨水同位素组成资料，讨论了季风气候对雨水同位素组成的影响。
6) 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。
参考词条
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。