助手标题  
全文文献 工具书 数字 学术定义 翻译助手 学术趋势 更多
查询帮助
意见反馈
   model 在 气象学 分类中 的翻译结果: 查询用时:0.211秒
图标索引 在分类学科中查询
所有学科
气象学
计算机软件及计算机应用
基础医学
数学
石油天然气工业
宏观经济管理与可持续发展
自动化技术
企业经济
环境科学与资源利用
更多类别查询

图标索引 历史查询
 

model
相关语句
  模式
    The Application of GPS Observations on Mesoscale Numerical Weather Prediction Model
    GPS资料在中尺度数值预报模式中的应用研究
短句来源
    Research on the Error and Predictability of Climate Model
    气候模式的误差及其可预报性研究
短句来源
    Influence of Land Surface Boundary Condions (Such as LAI) on the Regional Climate Simulation and Preparation of Land Surface Remotely-sensed Parameters for Regional Climate Model (CWRF+CLM)
    陆面下边界对区域气候模拟的影响(LAI为例)及区域气候模式(CWRF+CLM)陆面遥感参数预处理研究
短句来源
    Study on Optimization of the Dust Model System and Quantitative Classification of Dust Events in East Asia
    沙尘模式优化与东亚沙尘天气量化分级研究
短句来源
    Studies of Predictability Problems for Zebiak-Cane ENSO Model
    Zebiak-Cane ENSO预报模式的可预报性问题研究
短句来源
更多       
  模拟
    Climate Model and Climate simulation
    气候模式与气候模拟
短句来源
    STUDY ON SIMULATING THE CONVECTIVE BOUNDARY LAYER WITH THE HIGHER-ORDER-CLOSURE MODEL
    高阶矩模式模拟对流边界层的可行性研究
短句来源
    A NUMERICAL SIMULATION OF ONE-DIMENSIONAL LAND-SURFACE PROCESS MODEL
    简易一维陆面过程的数值模拟
短句来源
    STUDY ON DYNAMIC MATHEMATICAL MODEL OF WEATHER (Ⅱ)——SIMULATION PROGRAM AND RESULTS
    动态气象数学模型的研究(二)——模拟程序与模拟结果
短句来源
    Monte-carlo Model simulates the Influence of Complex Terrain on Diffusion
    Monte-Carlo法模拟复杂地形对扩散的影响
短句来源
更多       
  模式的
    Research on the Error and Predictability of Climate Model
    气候模式的误差及其可预报性研究
短句来源
    Studies of Predictability Problems for Zebiak-Cane ENSO Model
    Zebiak-Cane ENSO预报模式的可预报性问题研究
短句来源
    A RANDOM SOLUTION OF MODEL FOR LONG-RANGE FORECAST
    长期预报模式的随机解
短句来源
    STOCHASTIC ANALYSIS OF ZERO-DIMENSIONAL CLIMATE MODEL BASED ON FOKKER-PLANCK EQUATION
    基于Fokker-Planck方程的零维气候模式的随机分析
短句来源
    A SCHEME COMPARATIVE TEST OF INITIALIZATION WITH WIND DATA FOR A LIMITED-AREA FORECAST MODEL
    有限区域预报模式的风场——初始化方案的试验(一)
短句来源
更多       
  “model”译为未确定词的双语例句
    A TEST OF VARIATIONAL INITIALIZATION FOR A BAROTROPIC PRIMITIVE EQUATION MODEL
    正压原始方程变分初值试验
短句来源
    An Experiment of Rainfall Measurement for a Single Locating with a Model 711-Storm-Detecting-Radar
    711测雨雷达进行单点降水测量的试验
短句来源
    Some Methods for Correction of Echo Data Measured by Model 711 Radar
    711雷达测定回波数据订正的方法
短句来源
    Experimental Study of Atmospheric Diffusion of the Jumping Model
    跃变型扩散的实验研究
短句来源
    A METHOD OF WEATHER FORECAST DONE BY RECEIVING AND COMPILING THE NUMERICAL PREDICTION PRODUCTS FROM MODEL 《 T42 》
    接收编辑国家《T42》数值预报产品作天气预报的一种方法
短句来源
更多       
查询“model”译词为用户自定义的双语例句

    我想查看译文中含有:的双语例句
例句
为了更好的帮助您理解掌握查询词或其译词在地道英语中的实际用法,我们为您准备了出自英文原文的大量英语例句,供您参考。
  model
Reductive group actions on affine quadrics with 1-dimensional quotient: Linearization when a linear model exists
      
A linear model for a given action is a linear orthogonal action with the same orbit types and equivalent slice representations.
      
We prove that if a reductive group action on an affine quadric with a 1-dimensional quotient has a linear model, then the action is linearizable.
      
Using the path model and the theory of crystals, we generalize the concept of patterns to arbitrary complex semi-simple algebraic groups.
      
In the model situationD is the Siegel disc,S is the manifold of Lagrangian subspaces andG is the symplectic group.
      
更多          


This is a brief report of a preliminary survey of certain rain-bearing systems over China in later spring and summer. In the first part, a general description of the methods of analysis used in this survey is given. As the temperature and wind fields are weak, and the precipitation is heavy, smaller intervals for the isotherms and contours in the constant pressure surface and pseudo-equivalent potential instead of potential temperature in the cross section analysis are used.In the second part, there are descriptions...

This is a brief report of a preliminary survey of certain rain-bearing systems over China in later spring and summer. In the first part, a general description of the methods of analysis used in this survey is given. As the temperature and wind fields are weak, and the precipitation is heavy, smaller intervals for the isotherms and contours in the constant pressure surface and pseudo-equivalent potential instead of potential temperature in the cross section analysis are used.In the second part, there are descriptions of the structure and development of five frequently observed rain-bearing systems i.e. cold front, blocking high and cold vortex, monsoon heat low, warm front and typhoon.The last part consists of discussions of some points of view in synoptic meteorology in China. It is stated that the monsoon precipitation is various in intensity and duration according the large-scale flow patterns. The difference of moisture content in the middle troposphere as a criterion for the identification of equatorial or tropical maritime air mass is proved to be missleading. It is shown that the upper air moist content is high only within the raining region near the polar or equatorial front. To the south of the equatorial front within the so-called equatorial air mass, the moist content in the middle troposphere is as low as within the tropical maritime air mass. It is the convergence and lifting of the tropical air mass which releases the convective instability and induces the surface moist air rising to the middle troposphere. The phenomenon of the forward-inclination of the so-called North-West Trough based on the time cross-section of wind is proved to be a mistake by combining two systems into one trough. The terminology of shear line, and the correct application of synoptic models in weather analysis and forecas-ting are also discussed.

本文是一年来从事夏季降水天气初步普查的简单报告。第一节首先指出所用分析方法与一般国内所通用者,稍有不同。高空等压面分析,取20米作为等高缐间隔,2℃作为等温缐间隔。代替40米及5℃的间隔,以适应夏半年较弱的温度场与气压形势场,在剖面分析中以等假相当位温缐代替位温缐,与等温缐配合以适应降水天气的凝结降水过程。 第二节讨论了五种夏半年基本降水天气系统,即冷锋、阻塞高压与冷涡、季风热低压、 暖锋及有风的结构,并简单地叙述了演变过程。 第三节对某些天气概念提供一些批判性的讨论。根据现已增加的观测材料,论证季风与梅雨是多样性的,决定于大规模的温度场与流场特性,以高空湿度大小区分赤道气团与热带海洋气团,证明是不适当的,因为中国赤道锋降水区域以南,即在所谓南南季风的赤道气团中,中层大气仍是干燥的。降水区域内,中层对流层的大量水份,是由于辐合或抬升的作用,使潜势的对流不稳定性成为现实的不稳定性,而由下层空气上升带上去的。文中还论证了所谓西北槽槽缐前倾是将两个系统混作—个系统的不正确桔果。最后还讨论了切交缐及一般模型在天气分析预报中的应用与限制。

Using a 2-parameter model a graphical method for predicting the height of BOO mb surface is given and practical operational, procedure is described. This method is much in accord with that given by Fj rtoft for barotropic model. For a case of intense development of cold wave we have computed three 500 mb prognostic charts for 24 hours interval It is found that the locations and intensities of the systems computed by this method are in reasonable agreement with the observed ones.

在本文中作者给出了用图解计算500毫巴24小时形势预告图的方法和实际操作步骤。应用这个方法作者计算了三张500毫巴预告图,结果和实况还大致相似。

Some 24 and 48-hr numerical forecasts for 500 mb topography over a part of Asiaare prepared by graphical method with a quasi-geostrophic two-parameter model.Theresult is in general rather good,but for the case of blocking,the negative height-change centersouth to the position of the blocking high is not forecasted and thus the blocking high doesnot appear on our prognostic chart.This is due to the neglection of the 500 mb divergence whichis of importance for the major development of weather systems on...

Some 24 and 48-hr numerical forecasts for 500 mb topography over a part of Asiaare prepared by graphical method with a quasi-geostrophic two-parameter model.Theresult is in general rather good,but for the case of blocking,the negative height-change centersouth to the position of the blocking high is not forecasted and thus the blocking high doesnot appear on our prognostic chart.This is due to the neglection of the 500 mb divergence whichis of importance for the major development of weather systems on 500 mb level.Some of theerrors is attributed to the Fjφrtoft's formula used for the graphical integration of Poissonequation.

作者用准地转两层模式以图解方法试作了24小时及48小时亚洲部分的500毫巴高度预报。从所作的几个例子来看,有的预报结果较好,但像阻塞高压的一个例子中高压位置南边的负变高没有预报出来,因此预报图上没有阻塞高压的形成。原因主要是在准地转两层模式没有恰切地考虑到500毫巴的辐散场。作者指出500毫巴上天气系统有猛烈发展时500毫巴上的辐散场是比较大的,要考虑到后者的作用就必须应用三层模式或不用准地转假定。作者并指出了 Fj(?)rtoft 的图解方法也有不小的误差。

 
<< 更多相关文摘    
图标索引 相关查询

 


 
CNKI小工具
在英文学术搜索中查有关model的内容
在知识搜索中查有关model的内容
在数字搜索中查有关model的内容
在概念知识元中查有关model的内容
在学术趋势中查有关model的内容
 
 

CNKI主页设CNKI翻译助手为主页 | 收藏CNKI翻译助手 | 广告服务 | 英文学术搜索
版权图标  2008 CNKI-中国知网
京ICP证040431号 互联网出版许可证 新出网证(京)字008号
北京市公安局海淀分局 备案号:110 1081725
版权图标 2008中国知网(cnki) 中国学术期刊(光盘版)电子杂志社