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cloud microphysical process
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  云微物理过程
     THE CLOUD MODEL OF TWO-DIMENSIONAL ANELASTIC NON-STATIC EQUILIBRIUM: PART ONE-REGARDING THE INFLUENCE OF CLOUD MICROPHYSICAL PROCESS IN LOW-LEVEL WIND SHEAR
     二维滞弹性非静力平衡云模式第一部分──低空风切变对云微物理过程的影响
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  云物理的
     The output of the new scheme could give reasonable microstructure of cloud and indicate some characteristics of stratus cloud, which enhances the capability of MM5 to study the cloud microphysical process.
     模拟给出了云的合理微观结构,揭示了层状云的一些特征,增强了MM5研究微观云物理的能力;
短句来源
     The output of the new scheme can give reasonable microstructure of stratus cloud and indicate its some characteristics, which enhance the capability of MM5 to study the cloud microphysical process.
     模拟结果给出了层状云的合理微观结构和它的一些特征,增强了MM5研究微观云物理的能力;
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  “cloud microphysical process”译为未确定词的双语例句
     Using the 1AP 3-D hailstorm numerical model, we analyze influence of variation on rainfall amount, hail fallout amount, dynamical process of cloud, microphysical process, mechanism of hail suppression with seeding, and seeding outcome.
     本文利用中国科学院大气物理研究所的三维冰雹云催化数值模式,通过对冰雹云的模拟和对谱参数的数值试验结果,分析了冰雹云中粒子谱形的变化,对云和降水过程的影响,其中包括雨滴谱、冰晶谱、霰谱的形状参数对自然云的发展过程、降雨降雹、云中微物理过程、霰以及冰雹的形成机制的影响。
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  相似匹配句对
     In the process of the E.
     E.
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     process.
     工艺的优劣分析。
短句来源
     THE MICROPHYSICAL STRUCTURE OF SNOW CLOUD AND THE GROWTH PROCESS OF SNOW IN WINTER IN XINJIANG
     新疆冬季降雪微结构及其增长过程的初步研究
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     THE CLOUD
     云
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     Process Technology of Satellite Cloud Atlas
     卫星云图处理技术
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  cloud microphysical process
The cloud microphysical process of the principle model has been defined.
      


three dimensional model of stratiform cloud system is constructed by mesoscale atmospheric model of Anthes et al. and two-parameter stratiform cloud model of Hu et al. which include three phases of water and detailed cloud microphysical processes. The hybrid-scheme and the time-split scheme are used for calculating the microphysical processes. A Lagrangean scheme is designed for calculating the falling of particles. The simulated results of 2 mesoscale vortex cases using this model...

three dimensional model of stratiform cloud system is constructed by mesoscale atmospheric model of Anthes et al. and two-parameter stratiform cloud model of Hu et al. which include three phases of water and detailed cloud microphysical processes. The hybrid-scheme and the time-split scheme are used for calculating the microphysical processes. A Lagrangean scheme is designed for calculating the falling of particles. The simulated results of 2 mesoscale vortex cases using this model are analyzed and compared with other models. It is shown that more resonable simulated structures of circulation, cloud system and surface precipitation can be given by this model.

在Anthesetal.的中尺度模式基础上引入胡志晋的双参数层状云模式并重新编制了程序,构成一个包含三种水相态和比较详细云物理过程的三维层状云系模式。为保持在较长时步中计算的稳定和精度,对微物理过程的计算采用混合格式,少数过程采用时间分裂格式,在相变过程的处理上设计了同时计算不同相态相变的参数化方案,按Lagrangian方法设计了粒子下落格式。用干模式、积云参数化模式、两相显式模式和本文模式对两个中尺度低涡个例作了模拟,对比分析不同模式的模拟能力。结果表明本文模式对涡环流结构、云场和降水分布的摸拟比其他模式更合理,更接近实况。

A cloud model of two-dimensional time- (lependent has been used to study the effectsof middle and low-level wind shear on convection in this paper. And five schemes are de-signed to use in the comparative test. The result indicates: when the middle and low -levelwind shear is small, it is easy to lead to convection. When the middle and low-level windshear doesn' texceed a certain value, the convection develops slowly, but at last the severeconvection is caused to outbreak. Otherwise the convection doesn'...

A cloud model of two-dimensional time- (lependent has been used to study the effectsof middle and low-level wind shear on convection in this paper. And five schemes are de-signed to use in the comparative test. The result indicates: when the middle and low -levelwind shear is small, it is easy to lead to convection. When the middle and low-level windshear doesn' texceed a certain value, the convection develops slowly, but at last the severeconvection is caused to outbreak. Otherwise the convection doesn' t develop. On the otherhand, the middle and low-level wind shear can strengthen cloud microphysical processes andsurface precipitation,

本文运用已建立的二维时变云模式[1],就中低空风垂直切变对对流和云微物理过程的影响进行了模拟研究。为此设计了五种方案进行了对比试验。结果表明:中低空风切变较小时,容易爆发对流;中低空切变不超过某一值时,对流发展缓慢,但最终会爆发强对流;一旦中低空风切变超过某一值时,则对流发展不起来。另一方面,中低空风切变可加强各云微物理过程及地面降水量。

According to physical analysis;; cloud microphysical parameterizations;; iarge-scaledynamical proeess and cloud cover should be considered on the prognostic schemes for non-convectiveclouds in GCM. Then;; it is reviewed and discussed that the condensation (deposition) process;; includingthe large-scale adjustment's method;; the large-scale closure's method and statistics;; method;; and somemodifications should be considered. For the Bergeron process;; the non-linear process should be consid-ered. For the other...

According to physical analysis;; cloud microphysical parameterizations;; iarge-scaledynamical proeess and cloud cover should be considered on the prognostic schemes for non-convectiveclouds in GCM. Then;; it is reviewed and discussed that the condensation (deposition) process;; includingthe large-scale adjustment's method;; the large-scale closure's method and statistics;; method;; and somemodifications should be considered. For the Bergeron process;; the non-linear process should be consid-ered. For the other cloud microphysical process;; some new schemes should be adopted;; instead of usingthe meso-scale cloud model directly. On the future model;; Sc from Cu should be considered. For Cifrom Cu;; some modifications should be considered. At last;; the new cloud cover prognostic methods inGCM are suggested from Lagrange view;; free-boundary view and staticstics view on the basis ofmathamatical-physics method.

通过对大气环流模式中非对流云预报方法的物理分析表明:大气环流模式中非对流云的预报,应包括非对流云的云水(冰)微物理过程参数化、大尺度动力过程和云量三个方面。从大尺度调整法、大尺度闭合法和统计方法三个方面,讨论了已有的大气环流模式中非对流云的凝结(华)过程的参数化方案,指出了存在的问题及改进方法。对于Bergeron过程,指出了已有的线性化经验公式的不足,强调了采用非线性参数化公式的重要性。本文指出了直接将中尺度模式搬到大尺度模式是不合适的,有必要进一步研究。同时指出将来的大气环流模式,应考虑浅积云所产生的层积云,还分析了已有的深积云对流所产生的高空卷云的参数化公式。并从Lagrange观点、动边界观点和统计观点,提出了大气环流模式中的云量预报的一些方案,并指出了已有方案的不足。

 
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