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强对流     
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  severe convection
     Analysis on Severe Convection Weather on June 21,2005 in Henan
     河南省2005-06-21强对流天气分析
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     Analysis for the Factors and Forecast of Severe Convection Weather on April 5th, 2002
     2002年4月5日罕见的强对流天气成因及预报分析
短句来源
     The Numerical Simulation and Diagnosis Research of Rainstorm and Severe Convection Weather in Northeast China
     东北地区暴雨、强对流天气的数值模拟诊断研究
短句来源
     NUMERICAL DIAGNOSIS OF INFLUENCE OF MESOSCALE TERRAIN ON SEVERE CONVECTION WEATHER
     中尺度地形对强对流天气的影响的数值诊断
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     The Radar Echo Analysis and Forecasting on Severe Convection Weather
     强对流天气的雷达回波分析与预报
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  strong convection
     Analysis on the "02.4.5" Strong Convection Weather process in Guangxi
     广西“02.4.5”强对流天气过程分析
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     Analysis of “5,May,1999" Strong Convection Weather Process of Lanzhou
     1999年5月5日兰州强对流天气分析
短句来源
     Application of Forecast Field of T106 Physical Factor On Locating Strong Convection Weather
     T106物理量预报场在强对流天气落区预报中的应用
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     Analysis of the "0418" Strong Convection Weather in JiaXing and the Starting Point of Forecast
     嘉兴市“0418”强对流天气分析和预报着眼点
     Analysis also finds out that the 0℃ layer is nearby 700 hPa altitude and indexes of △θse and Sweat are of strong significance for the occurance and development of strong convection weather.
     分析发现0℃层在700hPa附近,△θse、Sweat指数对强对流发生发展有重要指示意义。
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  severe convective
     Application of Environmental Parameters E_(CAP) and I_(EH) to the Analyses of the Severe Convective Weather
     E_(CAP)等环境参数在强对流天气分析中的应用
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     Application of Lap-3000 boundary wind profile radar to severe convective weather forecast
     上海LAP-3000边界层风廓线雷达在强对流天气预报中的应用初探
短句来源
     Analysis of “06.4” severe Convective Weather Process in Fuzhou,Jiangxi Province
     抚州市“06.4”强对流天气过程分析
     AN ANALYSIS OF THE 95.7.19 SEVERE CONVECTIVE STORM IN PINGLIANG
     平凉“95.7.19”强对流风暴分析
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     Application of Data at 925hPa Standard Pressure Level to Severe Convective Weather Forecasting
     925hPa标准等压面资料在强对流天气预报中的应用
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  strong convective
     An Analysis on the “12.19” Strong Convective Weather in Jiangmen
     江门“12.19”强对流天气分析
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     The precipitation efficiency of strong convective cell is the biggest,the mean value of which is 25.74%,and is 15.74% more than convective cell and 13.21% than normal convective cell.
     强对流单体的降水效率最大,平均值为25.74%,比对流单体多15.74%,比合并对流单体多13.21%。
短句来源
     The result indicates that Merger convective cell's liquid in its whole lifetime 269.76×106 m3.fewer than strong convective cell,and 198.68×106 m3.more than normal convective cell.
     分析结果表明,合并对流单体整个生命期间的液态含水量,比强对流单体液态含水量少269.76×106m3,比对流单体多198.68×106m3。
短句来源
     An Analysis of "5·11" Strong Convective Weather Occurrence in Shenzhen Using V-3θ Diagrams
     深圳“5.11”强对流天气的V-3θ图分析
短句来源
     Analysis On The Strong Convective Process Occurred On April 5 2002 In Jiangxi
     2002年4月5日江西强对流天气过程分析
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  severe convection
The prediction of two cases of severe convection: implications for forecast guidance
      
Severe convection in the Sydney basin regularly produces destructive winds, heavy rain or flash flooding, and damage from large hail.
      
Initial work has been carried out that examines two cases of severe convection in the Sydney basin.
      
The model results discriminated well between severe convection that actually did occur in the first case (1 December, 2000) and the failure of severe convection to develop in the second case (8 December, 2000).
      
The operational forecasters predicted severe convection to occur in both cases.
      
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  strong convection
The difference is examined in atmospheric circulation and Sea Surface Temperatures (SSTs) in the trop-ics and subtropics between weak and strong convection over the tropical western Pacific warm pool (signified as WPWP).
      
A composite study was carried out to examine the differences in atmospheric circulation and SSTs between weak and strong convection over WPWP.
      
A simulation study of ionization depletion in the auroral ionosphericF-region caused by strong convection electric field
      
THe effects of strong convection electric field on the electron density in the auroral ionosphericF-region have been simulated numerically by means of a physical model.
      
The strengthened meridional temperature gradient enhances the Asian summer monsoon circulation and favors the strong convection.
      
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  severe convective
The real time operational severe convective weather forecast experiment carried out during May to July in 1990 over the Changjiang Delta is briefly described.
      
The heavy rainfall and severe convective weather forecast worksheets for the Changjiang Delta have been proposed and used in the daily forecasting.
      
On the helicity dynamics of severe convective storms
      
These cells are generally related to severe convective weather occurrences such as thunderstorm wind gusts, hail and tornados.
      
The predictand is the probability of a thunderstorm cell to generate severe convective weather events.
      
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  strong convective
The influence of horizontally non-uniform heating upon the development of strong convective mesoscale disturbances
      
It is shown by observational data and synoptic analysis that the development of strong convective echo is influenced by the horizontally non-uniform heating, such as the one caused by lake-land distribution.
      
One of the intriguing findings which accords well with observations demonstrates that cold currents create strong convective weather, while warm currents bring about stable weather: produce prolonged low clouds or fogs.
      
After onset of the SW monsoon the strong convective area moves northwards, while the SCS rain band moves to the center and north.
      
It is found that strong convective cells with reflectivity greater than 30dBZ mainly are situated in the front region of hailstorms, whereas the trailing stratiform region is in the rear part of the hailstorms.
      
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