积云对流

  • 网络Cumulus convection
积云对流积云对流
  1. 用积云对流方法计算MCC的降水

    MCC Rainfall Calculation Based on cumulus convection scheme

  2. 使用1979年1月至1984年12月向外长波辐射(OLR)资料,对热带地区积云对流的长期变化特征进行了研究。

    Using OLR data of 1979 to 1984 , the long-term variation features for cumulus convection over the tropical region are studied .

  3. 积云对流对ITCZ区域位涡的垂直输送

    Vertical transport of potential vorticity due to cumulus convection in the ITCZ area

  4. 积云对流加热的垂直差异对CISK的影响

    The influence of different vertical distribution of cumulus heating on CISK

  5. RIEMS中积云对流参数化方案对我国降水的影响

    Impact of Convective Parameterization on RIEMS Simulation of Summer Precipitation

  6. 四种积云对流参数化方案模拟的海平面气压场差别较大,其中GR方案较好地模拟出造成这次暴雨的高低压系统和中尺度气旋。

    The simulative sea level pressure of four CPSs showed large difference , in which the GR scheme had better simulated the high , low systems and mesoscale cyclone .

  7. 经验正交函数(EOF)分析的主要空间型反映了赤道中太平洋、热带西太平洋、阿拉伯海和副热带西太平洋地区的积云对流活动存在一定的关系。

    The EOF analysis indicates the relationship of the cumulus convection between equatorial middle Pacific , tropical western Pacific , the Arabian Sea and subtropical western Pacific .

  8. LTC登陆后保持一定强度,并从外界获得热量和水汽补充来支持积云对流发展,而积云对流对LTC的维持具有正反馈作用。

    LTC would draw heat and vapor from outside of the cyclone that would help LTC to develop cumulus convection in its circulation .

  9. 通过对强暴雨过程Q1和Q2的诊断,可为改进积云对流参数化中加热和增湿廓线提供可靠的物理依据。

    The reliable physical proof for improving heating and moisturizing profiles in the cumulus convective parameterization can be obtained through diagnosing Q1 and Q2 of the rainstorm event .

  10. QD和QL水平散度的垂直分布及其随时间的演变表明,动力学强迫总是位于对流层低层,而非绝热过程的强迫主要位于对流层中层,它与积云对流过程中的潜热反馈有关;

    The divergence of QD and QL 'S cross section analysis indicated that the dynamic forcing was located in low level of troposphere and the forcing of diabatic process was related with the release of latent heat ;

  11. 南海季风低压是通过积云对流和大尺度环境场的反馈作用而发展增强的,可认为,CISK机制是低压发生发展的主要机制。

    The development of the depression attributes to the feedback between cumulus convection and the largescale environment field . The genesis and development of the depression can be explained by CISK mechanism .

  12. 利用一个全球五层大气环流谱模式,试验和比较了三种不同积云对流参数化方案,即Manabe方案、Kuo方案和Arakawa-Schubert(A-S)方案,对全球气候数值模拟的影响。

    In this paper , a 5-level AGCM is used to examine and compare the influence of three kinds of convective parameterization schemes ( Manabe 's scheme , Kuo 's scheme and Arakawa-Schubert ( A-S ) scheme ) on the numerical simulation of global climate .

  13. 积云对流中扰动压力效应的诊断分析

    Diagnostic analysis of the effect of perturbation pressure on cumulus convection

  14. 积云对流凝结加热和云天辐射;

    The cumulus convective condensation heating and the radiation with cloud ;

  15. 积云对流参数化方案在热带大气季节内振荡模拟中的重要性

    Importance of cumulus schemes to numerically simulated tropical intra-seasonal oscillations

  16. 热带地区积云对流的长期变化特征

    Long-term variation features for cumulus convection over the tropical region

  17. 引入考虑凝结作用的连续性方程与积云对流参数化方案修正

    Continuity Equation Considering Condensation Effect and Modification of Cumulus Convection Parameterization Scheme

  18. 郭型积云对流参数化方案的对比试验及潜热加热效应

    Comparison experiments of Kuo type cumulus parameterization schemes and latent heating effects

  19. 积云对流与西南低涡的活动

    Cumulus convection and its relation to the SW China and Qinghai-Xizang Plateau vortexes

  20. 积云对流在非地转非线性斜压扰动发展中的作用

    The role of cumulus convection in the development of NoN-GEOSTROPHIC and non-linear baroclinic disturbance

  21. 台湾锋前暖区一次积云对流过程

    On a cumulus convection process in the pre frontal warm sector over Taiwan area

  22. 积云对流参数化技术

    A review on the cumulus convective parameterization

  23. 积云对流和冰雹天气不稳定能量的积累

    The relation between cumulus convection and the accumulation of unstable energy in the hail storm

  24. 下曳气流在积云对流中的作用

    The Role of Downdrafts in Cumulus Convection

  25. 辐射和积云对流过程对大气辐射通量的影响

    The impacts of the radiation and cumulus convective parameterization on the radiation fluxes in SAMIL

  26. 大气凝结水汽汇、凝结潜热作用与积云对流参数化

    Vapor sink and latent heat of condensation in the atmosphere and the parameterization of cumulus convection

  27. 中国夏季不同强度降水模拟对不同积云对流参数化方案的敏感性研究

    Sensitivity of Simulation of Different Intensity of Summer Precipitation over China to Different Cumulus Convection Parameterization Schemes

  28. 热带积云对流加热在全球大气遥响应中的重要作用&数值试验结果

    The importance of tropical convection heating in the global atmospheric remote response ─ a numerical simulation study

  29. 积云对流凝结加热和洋面上的潜热感热通量;

    The cumulus convective condensation heating and the latent and sensible heat fluxes on the sea surface ;

  30. 热带海洋上积云对流

    Cumulus convection over tropical ocean