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干对流
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  “干对流”译为未确定词的双语例句
     The use of this scheme has made the avoidance of the hydrostatic unstable which occured in the upper layer when the original limited layer dry convective adjustment scheme for T, q and V was used, and allowed us to carry the integration of the model over a much longer period. The simulated distributions of the precipitation rate are also improved.
     此方案的采用避免了该模式过去采用有限层T、q、V的干对流调整方案时所产生的上层的静力不稳定现象,延长了对方程组的积分期限,而且模拟的降水率分布也有所改善。
短句来源
     Based on a simplified dry boundary layer convection model and the nonlinear ther-modynamic theorem, the dynamical and thermodynamical characteristics for forming, develop-ing and decaying boundary layer eddies are studied.
     利用简化的边界层日变化干对流模式,结合非线性热力学观点,数值模拟并分析了日间对流边界层中大涡形成、发展及衰亡的动力和热力学特征.
短句来源
  相似匹配句对
     A COMPARATIVE TEST OF THE DRY ADIABATIC ADJUSTMENT SCHEMES
     绝热对流调整方案的对比试验
短句来源
     (stem leaven).
     g(曲)。
短句来源
     (g(dry membrane) ) ?
     (g(膜))?
短句来源
     THE DIFFERENCE OF INFLUENCE OF DRY AND MOIST CONVECTION ON CIRCUMSTANCE
     中尺度、湿对流影响环境场的差异分析
短句来源
     Determination of Cooling Curve at Convection
     对流冷却的测定
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  dry convection
Both the dry convection north of 15°N in the heat low (mainly in June-July) and deep convection in the ITCZ (in August-September) are modulated by the 3-5-day easterly waves over the land.
      
The heated air rises via dry convection, creating a positive temperature anomaly in the mid-to-upper troposphere over the TP relative to the region to the south.
      
Thickness of the dry convection and large-scale subsidence above deserts
      
Thickness of dry convection above various deserts of the world is obtained from aerological data, and assimilated data from ECMWF.
      
A Simple Mixing Length Formulation for the Eddy-Diffusivity Parameterization of Dry Convection
      
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A convective adjustment scheme developed for the p-σ combined vertical coordinate five-layer primitive equation model is presented in detail in this paper. Besides the temperature, the humidity field is also adjusted with this scheme. The use of this scheme has made the avoidance of the hydrostatic unstable which occured in the upper layer when the original limited layer dry convective adjustment scheme for T, q and V was used, and allowed us to carry the integration of the model over a much longer period. The...

A convective adjustment scheme developed for the p-σ combined vertical coordinate five-layer primitive equation model is presented in detail in this paper. Besides the temperature, the humidity field is also adjusted with this scheme. The use of this scheme has made the avoidance of the hydrostatic unstable which occured in the upper layer when the original limited layer dry convective adjustment scheme for T, q and V was used, and allowed us to carry the integration of the model over a much longer period. The simulated distributions of the precipitation rate are also improved.

本文较详细地介绍了为p-σ五层原始方程模式设计的一个对温度场作整层对流调整的方案。在温度场调整的同时,湿度场也相应受到调整。此方案的采用避免了该模式过去采用有限层T、q、V的干对流调整方案时所产生的上层的静力不稳定现象,延长了对方程组的积分期限,而且模拟的降水率分布也有所改善。

Based on the past studies on the relationship between the heating of the Tibetan Plateau and the onset of the East Asian monsoon,a review was given in this paper as part of the preparation task of the coming SCS MONEX.The air above the Plateau is a relative heat source in all seasons compared with the air over the surrounding areas at the same level and the same latitude.The major souce of the heating above the Plateau is provided by the sensible heat transports with the mechanism of the dry thermal convection...

Based on the past studies on the relationship between the heating of the Tibetan Plateau and the onset of the East Asian monsoon,a review was given in this paper as part of the preparation task of the coming SCS MONEX.The air above the Plateau is a relative heat source in all seasons compared with the air over the surrounding areas at the same level and the same latitude.The major souce of the heating above the Plateau is provided by the sensible heat transports with the mechanism of the dry thermal convection rising from the heated plateau surface,which produces the tropospheric heating over the Plateau.But the contribution from the precipitation is also important in the rainy season when the cumulus convection plays a significant role in the heating over the southeastern Plateau.The diabatic heating over the eastern Plateau is the primary cause of mid May atmospheric warming from the eastern Plateau to the centrl China Plain,which leads to the reversal of the meridional temperature gradient of the troposphere east of 80°E,which results in the commencement of the East Asian monsoon.

各季节青藏高原地面的感热加热相对周围地区强烈的辐射冷却而言始终是个热源.地面向上的感热输送是高原大气热源的主要贡献者(干对流输送),但在雨季潜热的贡献同样重要.东亚季风爆发时高原东南部地区对流层大气爆发性增暖的主要原因是高原东南部的非绝热加热作用;而这种增暖使得高原东部以南的温度梯度改变,从而导致风压场的调整——东亚季风爆发

Based on a simplified dry boundary layer convection model and the nonlinear ther-modynamic theorem, the dynamical and thermodynamical characteristics for forming, develop-ing and decaying boundary layer eddies are studied. As a result, large eddies in the convection boundary layer are always in an unsteady manner. Eddies merge and broken process existed si-multaneously during the evolution of convection boundary layer, the former corresponds to local entropy-decreasing, but the latter is accompanied with total...

Based on a simplified dry boundary layer convection model and the nonlinear ther-modynamic theorem, the dynamical and thermodynamical characteristics for forming, develop-ing and decaying boundary layer eddies are studied. As a result, large eddies in the convection boundary layer are always in an unsteady manner. Eddies merge and broken process existed si-multaneously during the evolution of convection boundary layer, the former corresponds to local entropy-decreasing, but the latter is accompanied with total entropy increasing. Eddies developing process can be viewed as the competition between two factors of total entropy increasing and local entropy-decreasing in the convection boundary layer.

利用简化的边界层日变化干对流模式,结合非线性热力学观点,数值模拟并分析了日间对流边界层中大涡形成、发展及衰亡的动力和热力学特征.结果表明,对流边界层中大涡始终处于不稳定状态,大涡的自组织合并和破碎串级输送过程同时并存,前者与边界层系统的局部减熵相对应,后者与对流边界层的总体增熵效应对应;大涡的演变是对流边界层总体增熵这一稳定因素和局部减熵这一不稳定因素相互竞争的结果.

 
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