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气压场的英文

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"气压场"怎么读用"气压场"造句

英文翻译手机手机版

  • baric field
  • field of pressure
  • pressure field

例句与用法

  • A preliminary study of the northern winter slp climate base state and its climate variability and effects
    北半球冬季海平面气压场的气候基本态与气候变率特征及其影响的初步研究
  • The baric field and the tempreture field of high latitude will have some changes because of the change in the vegetation states of the landuse
    由于下垫面植被状况的变化,高空气压场和温度场也随之发生一些变化。
  • And the dv of lower - level systems , e . g . , jet stream , is among the intermediate changes happening after the dv is displayed in the meiyu pressure field
    低空急流等系统的日变化是梅雨天气系统内,低层气压场形势出现日变化后发生的众多中间变化过程之一。
  • The system uses the arrowhead to express the speed vector of wind field and uses the contour line and color cloud to express the height of wave field
    风场风速矢量场采用方向箭头实现可视化,并且可同步显示气压场信息,海浪场可视化采用等高线、彩色云图、文本数值输出,也可实现风场同步。
  • By using the theoritical analysis , we study the nonlinear interaction between the storm surges and the astronomical tides and the theoritical mode of the storm surges under the control of the wind stress field and the wind pressure field in this paper
    本文运用理论分析的方法研究了风暴潮与天文潮的非线性相互作用以及风场、气压场作用下的风暴潮波的物理机制问题。本文共分为四章。
  • With the development of visualization in scientific computing , visualization is widely applied in the analyzing of the engineering computing . adopting the method ( being made up of real time air pressure field data , the method for numerical wind forecasting and the method for numerical wave forecasting ) of wind wave forecasting this paper presents the system of wind wave forecasting and its visualization , which is relevant with the finite difference method , visualization part is the main work of this paper
    随着科学计算可视化技术的发展,可视化在工程计算结果的分析中得到了广泛的应用,本文应用由实时预报气压场资料、海上风的数值预报模式、风浪数值预报模式三者构成一种风浪预报方法,结合有限差分方法,编制了风浪预报可视化系统,其中可视化部分是本文的主要工作。
  • 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。
  • Its interannual variation ' s main period is about 4 ~ 5a and the 7 ~ 8a ' s period exist too ; the interdecadal variation ' s main period of the australian high is about 15a . the interannual variation of australian high ( aah ) has correct correlation with antarctic oscillation and enso , and the enso ' s 4a period has the most important influence on the aah . ( 2 ) when the ah becomes stronger , the members of the whole aamcs are stronger following it . that is to say , in the years that the ah is stronger ( compared to the weak years of ah ) and on the horizontal circulation , the members of aamcs , including the ah , the cross - equator flow ( cef ) between 100 and 160 e , the south china sea south - west monsoom ( ssm ) , the south sea monsoon rough , the tropical easily flow , subtropical high ( sh ) , the mei - yu front , the mid - latitude effect , become stronger , and their positions are more southward ; in the meridional - right circulation , there are five circulations including classic monsoon meridional - cirle circulation and hadley circulation that become stronger in the strong years of ah than in the weak years of ah
    本文采用ncep ncar再分析月平均的全球海平面气压场、高度场、海表温度场、高云量和cmap全球降水资料,以及中国160站逐月降水资料,分析了1948 2002年期间澳大利亚高压(以下简称澳高)的年际和年代际变化以及澳高年际变化对亚澳季风环流系统的影响,结果显示: ( 1 )澳高存在明显的年际和年代际变化,澳高年际变化以4 5年的周期变化为主,同时兼有7 8年左右的周期,而澳高的年代际变化则以15年左右的周期变化为主:澳高年际变化同时与南极涛动和enso有正相关,并且enso的4年左右的周期变化对澳高年际变化影响最大。
  • In addition , the ao index released by american climate prediction center ( cpc aoi ) fails to reflect the summer ao mode . in this paper , the time series of the leading principal component of the summertime ( june - september ) surface level pressure anomaly field over the domain poleward of 20 n is defined as the summertime ao index
    此外,美国气候预测中心发布的全年北极涛动月指数不能表现夏季北极涛动型,本文将北半球热带外地区( 20 n以北)夏季( 6 - 9月)海平面气压场eof主模态的时间序列定义为夏季北极涛动指数。
  • By using the data from 9210 broadcast system and t213 numeric forecast re - analysis data , we studied the starting and developing of one necw , and discussed the mechanism of west - liaoning rainstorm at a definite necw circumstance . we can see , although the necw is weather scale system , the distribution at difference level contacts very important information
    从分析中可以看出,虽然东北冷涡是天气尺度系统,但是由于气压场形势的配置不同、冷涡中心的位置和冷空气的移动方向不同、高低空气压场形势演变等原因,造成的局地天气差别是很显著的。
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