HLAFS显式云降水方案及其对暴雨和云的模拟(II)暴雨和云的模拟被引量：14

EXPLICIT CLOUD SCHEMES OF HLAFS AND SIMULATION OF HEAVY RAINFALL AND CLOUDS, PART II: SIMULATION OF HEAVY RAINFALL AND CLOUDS

下载PDF

导出

摘要在HLAFS业务数值预报模式的动力框架下 ,利用文章 (I)所述的显式云降水方案 ,对一次暴雨过程和伴随着的云物理过程进行了模拟研究和分析。模拟结果表明 ,显式方案对降水落区和强降水中心位置的预报较原HLAFS的大尺度饱和凝结方案有明显改进。模式能合理地揭示出暴雨发生、发展过程中的云系演变规律和云物理过程。冰相过程对降水、中尺度热力和动力场有明显影响 ,特别是冰相过程有利于降水的早期的形成速率。与卫星TBB资料的对比分析表明 ,引进显式方案后 ,模式能较合理地模拟出云系的轮廓、位置、范围、强度、生消和移向 ,模式模拟出的云顶温度与卫星测量出的云顶温度较为一致。 Based on the explicit cloud schemes described in Part I, a heavy rainfall event is simulated and analyzed within the dynamical framework of HLAFS. The results show that including explicit cloud schemes in a mesoscale model improved the heavy rainfall forecast and the understanding of its mesoscale characteristics obviously. The simulation results of the explicit schemes were better than that of the old diagnostic cloud scheme of HLAFS for rainfall location. The mesoscale model including explicit schemes is able to reveal the cloud field evolution and cloud physical characteristics during heavy rainfall development. Ice phase cloud microphysics processes have significant effects on mesoscale processes and their thermal and dynamical structure, especially for precipitate production and maintenance of heavy rainfall during its early developing stage. The outline, location, strength, scale, formation and dissipation, and moving direction of a cloud system are well simulated in general compared with satellite TBB data. The simulated cloud top temperature is in agreement with Satellite TBB.

作者刘奇俊胡志晋周秀骥

机构地区中国气象科学研究院

出处《应用气象学报》 CSCD 北大核心 2003年第b03期68-77,共10页 Journal of Applied Meteorological Science

基金 973项目"我国重大天气灾害的形成机理和预测理论研究" "十五"攻关"人工增雨技术研究及示范 (编号 :2 0 0 1BA6 10A - 0 6 )" "九五"攻关"人工增雨成套技术预研究"的共同资助。

关键词 HLAFS数值预报模式显式云降水方案云物理过程暴雨模拟降水落区卫星测量人工增雨技术 HLAFS Explicit prognostic cloud schemes Cloud physical processes Heavy rainfall simulation

分类号 P458.1 [天文地球—大气科学及气象学]

引文网络
相关文献

参考文献4

1国家气象中心.有限区数值预报业务系统(技术报告)[M].北京：国家气象中心,1994..
2刘奇俊,胡志晋,周秀骥.HLAFS显式云降水方案及其对暴雨和云的模拟(I)云降水显式方案[J].应用气象学报,2003,14(b03):60-67. 被引量：45
3Zhang D-L. The effect of parameterized ice micro-physics on the simulation of vortex circulation with a mesoscale hydrostatic model. Tellus, 1989, 41(A) : 132--147.
4Zhao Q, Carr E H. A prognostic cloud scheme for operational NWP model. Mon. Wea. Rev. , 1997, 125:19311953.

二级参考文献15

1.国家气象中心有限区数值预报业务系统(技术手册)[M].北京：国家气象中心,1994..
2胡志晋.严采繁层状云微物理过程的数值模拟:(一)微物理模式[J].中国气象科学研究院院刊,1986,1(1):37-52.
3Zhang D-L. The effect of parameterized ice micro-physics on the simulation of vortex circulation with a mesoscale hydro-static model. Tellus, 1989, 41(A) ," 132 -- 147.
4Hu Zhijin, He Guanfang. Numerical simulation of microphysical processes in cumulonimbus Part I: microphysicalModel. Acta Meteorological Sinica, 1988, 2(4): 471--490.
5Meyers M P, DeMott P J, Cotton W R. New primary ice-nucleation parameterizations in an explicit cloud model. J.Appl. Meteor., 1992, 31:708--721.
6Young K C. The role of contact nucleation in ice phase initiation in cloud. J. Atmos. Sci. , 1974, 31: 768--776.
7Bigg E K. The supercooling of water. Proc. Phys. Soc. London, 1953, B66, 688--694.
8Meyers M P. New RAMS cloud microphysics parameterization. Part Ⅱ: The two-moment scheme. Atmospheric Research, 1997, 45: 3--39.
9Cohard J M, Pinty J P. A comprehensive two-moment warm microphysical bulk scheme. I: Description and tests. Q.J. R. Meteor. Soc., 2000, 126: 1815--1842.
10Kong Fanyou, Yau M K. An explicit approach to microphysics in MC2. Atmosphere-Ocean. 1997, 35(3) : 257--291.