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Home > chinese-english > "zonal circulation" in English

English translation for "zonal circulation"

纬向环流
纬向环行
纬向气流


Related Translations:
zonal:  adj.1.成带的,带状的。2.区域[地区]性的。短语和例子zonal structure 【矿物】带状构造,环状构造。
zonal alteration:  带状蚀变
zonal axis:  晶带轴
zonal dislocation:  带状位错
zonal fare:  分区票价
zonal harmonics:  带调和带函数带谐涵数
zonal profile:  分带剖面综合剖面
zonal rectification:  分带纠正
zonal charge:  分区收费
zonal westerlies:  纬向西风西风带
Example Sentences:
1.Equatorial zonal circulation ; walker circulation
赤道纬向环流walker环流
2.The climatic characteristics of the equatorial zonal circulation retrieved with ir and wv channels on satellite
卫星双通道反演的赤道纬向环流的气候特征
3.Especially , t - test shows that significance of the asia polar vortex , zonal circulation index , the most northern extension edge of subtropical high of northern west pacific and the warm pool of pacific ocean , are at 95 % ( 90 % )
特别地,亚洲极涡、纬向环流指数、西太平洋副热带高压北界位置及太平洋暖池的海表面温度等因子均通过了95 % ( 90 % )信度水平检验。
4.With the wind , pressure and sea surface temperature ( sst ) data provided by ncep / ncar reanalysis project and excess length of day ( lod ) data provided by international earth rotation service ( iers ) , atmospheric angular momentum ( aam ) and its horizontal and vertical transportation are computed and analyzed , which are in accordance with maintenance of the zonal circulation . and the anomalous aam is highly consistent with el nino events
应用ncep / ncar40年再分析计划提供的风场、气压场、海温等资料以及国际地球自转服务局( iers )提供的日长变化资料,计算大气角动量及其水平、垂直输送,分析其气候及异常特征,发现角动量及其输送与纬向环流的维持相一致,角动量异常与厄尔尼诺事件紧密相关。
5.Climatic mean map , it is further confirmed that it s a good approach to retrieve the equatorial zonal circulation by using the ir indicate ascending branch and wv indicate descending branch channels . the definition of the index of zonal circulation with the olr and fwv are presented and the 17 years mean annual and seasonal equatorial circulation are drawn . the climatic characteristics of the equatorial zonal circulation are analyzed in detail . consequently the fore results of the other observation are corrected
通过波耳兹曼公式换算得到的6 . 7m水汽辐射通量密度,以便于与olr比较与ncep再分析的500hpa的年气候平均图进行比较,分析其异同,进一步证明了用卫星观测的红外,水汽双通道olr表示上升运动, fwv表示下沉运动去反演纬向垂直环流是一个极好的途径。
6.As a result , we find that in winter when the kuroshio is cooler than the normal , at following summer , the continental cyclone deepen and the east asia monsoon strengthen , that the mid - latitude blocking high weaken and zonal circulation develop , the east asia teleconnection of " - + - " is stired up , so that subtropical high weaken and diminish , and tend to east north , tropical monsoon trough strengthen and mei - yu front weaken , and tend to north , meanwhile south asia high weaken and diminish , and tend to eastvnorth , is easy to form eastern region type
结果发现当黑潮海温冷异常时,后期夏季大陆热低压加深,东亚夏季风偏强。中纬度阻塞高压减弱,东亚地区纬向环流发展,在东亚-西太平洋地区激发“ - + - ”的东亚遥相关型,从而西太平洋副高强度偏弱,面积偏小,位置偏东、偏北,东亚梅雨锋也偏弱,季风槽则变强,位置偏北。同时南亚高压偏弱,位置偏北、偏东,易形成东部型。
7.During 1950 ~ 1976 / 1977 , the walker circulation over the tropical pacific and the vertical zonal monsoon circulation over the tropical indian ocean coupled at the oceanic continent , the same period when el nino occurs , the anomaly of the west wind over the tropical pacific can correlate with the departure of east wind over the tropical indian ocean through the two coupled vertical zonal circulation . but after 1976 / 1977 , the updraft of the walker circulation moved eastward . locating at the north of australia . therefore the two vertical zonal circulation could n ' t coupled , and the anomaly of west wind and the departure of east wind could n ' t geared . in the result . the signal of enso decreased in indian ocean after 1976 / 1977
1951 1976 1977年,热带太平洋的walker环流和热带印度洋的纬向季风环流在海洋性大陆附近耦合,当elnino事件发生时,太平洋的西风异常可以通过这两个纬向的垂直环流与印度洋的东风异常联系起来,而1976 1977年以后,由于西太平洋walker环流上升支东移到澳大利亚北部,热带两洋的纬向垂直环流无法耦合,热带太平洋elnino事件中的西风异常与热带印度洋的东风异常联系减弱,所以1976 1977年以后, enso在热带印度洋的信号减弱了。
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