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对流     
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  convection
    ON THE LOCAL CONDITIONS OF CONVECTION DEVELOPMENT
    对流发展局部气象条件的初步理论分析
短句来源
    Warm Dry Lid and Severe Convection over the Southeast Coastal Region of China
    东南沿海的干暖盖与强对流天气
短句来源
    DIAGNOSTIC ANALYSIS OF THE EFFECT OF PERTURBATION PRESSURE ON CUMULUS CONVECTION
    积云对流中扰动压力效应的诊断分析
短句来源
    VERTICAL TRANSPORT OF POTENTIAL VORTICITY DUE TO CUMULUS CONVECTION IN THE ITCZ AREA
    积云对流对ITCZ区域位涡的垂直输送
短句来源
    ADVANCES IN RESEARCH OF CUMULUS CONVECTION PARAMETERIZATION SCHEME
    积云对流参数化方案研究的进展
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  convective
    Study on Mesoscale Strong Convective Weather in Xichang Satellite Launch Site
    西昌卫星发射场区中尺度强对流天气研究
短句来源
    THE STUDY OF TURBULENCE STRUCTURE COEFFICIENT IN THE CONVECTIVE BOUNDARY LAYER BY USING ACOUSTIC RADAR
    对流边界层湍流结构系数的声雷达研究
短句来源
    A CONVECTIVE ADJUSTMENT SCHEME FOR T AND q IN ENTIRE LAYER USED IN THE NUMERICAL MODEL
    在数值模式中的一个对T和q的整层对流调整方案
短句来源
    APPLICATION OF SODAR SOUNDING TO ATMOSPHERIC DISPERSION (3)-CALCULATION OF VERTICAL DIFFUSION COEFFICIENTS IN THE CONVECTIVE BOUNDARY LAYER
    声雷达探测在大气扩散研究中的应用(三)——对流边界层中垂直扩散系数的计算
短句来源
    Analysis of occurrence of squall line and commonly convective activity over North China
    华北平原飑线与一般对流活动发生条件的对比分析
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  advection
    Analising the ageostrophic wind on 200hPa level during Meiyu period in July 1 - 13, 1991,it showed that the wind was mostly set up by momentum exchange of cumulus convection, by the wind advection next.
    本文通过1991年梅雨后期,7月1—13日200hPa非地转场分析得出,梅雨期200hPa非地转风主要由积云对流动量转换形成。
短句来源
    The upper air divergence of troposphere,positive vorticity advection and lowlevel southeast jet make the mechanism responsible for the system's occurrence and development and the latent heat of condensation released from the convection contributes greatly to a further development and strengthening of it.
    对流层高层辐散、正涡度平流输送及低空东南急流是系统得以生成发展的机制,对流释放的凝结潜热对其进一步发展加强有重要贡献。
短句来源
    Three cases of the southwesterly low-level jet stream during the Meiyu season have been analyzed,showing that the kinetic energy of the jet stream is generated by the kinetic energy production of the divergence wind and the effect of the cumulus convection. The main physical factors affecting the rate of divergence wind kinetic energy production are latent heating, temperature advection and the role of the divergence term in the ω equation.
    本文分析了梅雨期内三次西南低空急流的实例,结果表明,散度风动能产生和积云对流效应是低中空急流的动能来源,而影响散度风动能产生的主要物理因子是潜热加热,温度平流以及ω方程中散度项的作用。
短句来源
    When the cold and warm advection is weak, the power-ful cumulus convection causes the south wind in the vicinity of the vortex and the nega-tive vorticity east of the vortex to increase, thus inhibiting the eastward motion of thevortex.
    当冷暖平流较弱时,强大的积云对流可使低涡附近的西南风分量加大,促使低涡东部负涡度加大,不利于低涡东移。
短句来源
    The results show that around the negative center of the difference between the upper and lower layers of generalized temperature advection will occure the severe convection weather.
    分析指出:广义温度平流上下层之差的负值中心附近是未来较强对流天气最可能出现的地区
短句来源
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  convections
    STABILITY ANALYSIS OF THE EQUATORIAL WAVES UNDER THE HEATING OF CUMULUS CONVECTIONS
    积云对流加热作用下赤道波的稳定性
短句来源
    Analysis and Nowcasting of Frequent and Severe Convections in Coastal North of Shandong Province
    鲁北沿海强对流天气多发的成因及临近预报
短句来源
    Meiyu Frontogenesis and Accompanying Convections
    梅雨锋生与锋面对流
    (4) The main factors which influence on strength of AGWs are activities of cold air and severe convections;
    (4)相关分析结果表明,影响大气重力波强度的主要因子是冷空气活动和强对流活动;
短句来源
    the tropical convections are strong in winter and spring, and weak in summer;
    热带对流活动冬春季偏强 ,夏季偏弱 ,夏季风偏弱 ;
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  convection
Mixed finite element method for the convection-dominated diffusion problems with small parameterε
      
for Sobolev equations with convection-dominated term
      
for linear Sobolev equations with convection-dominated term is given.
      
Thermally developing forced convection and the corresponding thermal stresses in a porous plate channel
      
We obtained the pattern of mantle convection for East Asia and the West Pacific.
      
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  convective
Radiative heat transfer in solids and convective heat transfer between the gas and the solid is especially studied.
      
Methods and algorithms of numerical simulation for three-dimensional thermal-convective motions of the inhomogeneous high-viscosity incompressible fluid in the direct and inverse time are described.
      
It is shown that, for univalent cations in the regime of convective diffusion, the coefficient of electrolyte rejection by the membrane correlates with the adsorption potential of cations (counterions) at the pore surface of a selective layer.
      
The gel-layer accumulates considerable surface and bulk charges and is characterized by the high hydraulic resistance hindering the convective ion transport.
      
It is shown that the effective mechanism of the saturation of nanocrystalline materials with impurities is their convective transfer by moving macrodislocations-linear defects of the regular packing of nanograins.
      
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  advection
The downward advection of trophogenic waters was found to create conditions for the extensive growth of microorganisms capable of decomposing and mineralizing organic carbon, nitrogen, and phosphorus in deep water layers.
      
The mixing of the seawater and groundwater occurs as a result of advection processes, the most important of which is wave percolation.
      
The equation of advection-diffusion transport of a reactive solute in a stream is solved by different methods.
      
A simple procedure is proposed for predicting this concentration based on an advection-diffusion model and field observational data.
      
Equations of flow in water-saturated porous medium and advection diffusion of dissolved salts are used to study salt transport and accumulation in subsoil water.
      
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  convections
Numerical analysis of thermal convections in a three-dimensional cavity: Influence of difference in approximation models on nume
      
The behavior of the critical temperature gradient is discussed in terms of various parameters of the system for both stationary and overstable convections.
      
Convections over Indo-China Peninsula and its surrounding areas further increase after the splitting.
      
UHI induced local air convergence and initiated the thunderstorm convections.
      
This isotopic constancy is incompatible with multiple, small, independent hydrothermal cells of the East Pacific Rise type, and fits much better with a model of hydrothermal convections driven by "magmatic floor heating".
      
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