Numerical study on the Water Vapor Transports of the TwoLandfalling Cyclones Affecting Hunan Province

YE Cheng-zhi-;LI Yun-ying;LI Zu-xian

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Plateau Meteorology
Plateau Meteorology ›› 2009, Vol. 28 ›› Issue (1) : 98-107.

Numerical study on the Water Vapor Transports of the TwoLandfalling Cyclones Affecting Hunan Province

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Abstract

Based on the multiple meteorological, hydrological intensify observations, and the NCEP reanalysis data, combined with the simulation and diagnosis data of meso\|scale numeric model of AREM, the water vapor features of two unique cyclone, the typhoon Bilis and Sepat which inducing heavy rainfall in the Hunan province are analyzed and some comparisons are conducted. The results show that, both of cyclones have two main water vapor channels, one is from south linkingwith the west\|south monsoon, and the other is from north linkingwith the cyclone′s low\|pressure circulation. In addition, their rain water mainly originates from the convergence of the lower levels, and is transported to the middle and high levels by local ascending airflows. However, it is noted that the water vapor flux in the Sepat′s heavy rain areas has stronger intensity than that of Bilis. Although with the weaker convergence of the water vapor flux and thinner convergent depth, Sepat′s lifetime is longer, total rainfall is larger and coveringarea is broader, since it has relatively stronger inner strength, and the steady wind shear in the south part of the cyclone′s center. On the otherhand, the main water vapor path of Bilis is much more southerly,the moisture convergence andthe interaction of the South China Sea monsoonarestronger than those of Sepat′s, its rain intensity in some areas and in certain periods is much more stronger.

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Typhoon Bilis and S / Feature of simulated / Water vapor transpor / Water vapor flux con

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YE Cheng-zhi- , LI Yun-ying , LI Zu-xian. Numerical study on the Water Vapor Transports of the TwoLandfalling Cyclones Affecting Hunan Province. Plateau Meteorology. 2009, 28(1): 98-107

References

[1]叶成志.“碧利斯”登陆后造成的湘东南特大致洪暴雨过程数值模拟研究[D]. 兰州大学硕士论文, 2007: 7-32
[2]陈联寿, 孟智勇. 我国热带气旋研究十年进展[J]. 大气科学, 2001, 25(3): 420-432
[3]陈联寿, 罗哲贤, 李英. 登陆热带气旋研究的进展[J]. 气象学报, 2004, 62(5): 541-548
[4]陈联寿, 徐祥德, 罗哲贤, 等.热带气旋动力学引论[M]. 北京: 气象出版社, 2002: 317
[5]郭荣芬, 鲁亚斌, 李燕, 等. “伊布都”台风影响云南的暴雨过程分析[J]. 高原气象, 2005, 24(5): 784-791
[6]张海霞, 崔晓鹏, 康凤琴, 等. 邯郸地区一次登陆台风大暴雨过程观测分析[J]. 高原气象, 2007, 26(5): 980-991
[7]康志明, 陈涛, 钱传海, 等. 0604号强热带风暴\!碧利斯\"特大暴雨的诊断研究[J]. 高原气象, 2008, 27(3): 596-607
[8]李英, 陈联寿, 王继志. 登陆热带气旋长久维持与迅速消亡的大尺度环流特征[J]. 气象学报, 2004, 62(2): 167-179
[9]刘子臣, 梁生俊, 张建宏. 登陆台风对黄土高原东部暴雨的影响[J]. 高原气象, 1997, 16（4）: 402-409
[10]林爱兰, 黄福均, 何光碧. 热带气旋与西南低涡相互作用的个例研究Ⅰ: 诊断分析[J]. 大气科学, 2002, 26(3): 352-360
[11]邓国, 周玉淑, 于占江. 台风Dan(9914)的水汽输送特征[J]. 热带气象学报, 2005, 21(5): 533-541
[12]张弘, 陈卫东, 孙伟. 一次台风与河套低涡共同影响的陕北暴雨分析[J]. 高原气象, 2006, 25（1）: 52-59
[13]郭达烽, 郑婧, 许爱华. 台风“碧利斯”的结构与江西暴雨诊断分析[J]. 气象与减灾研究, 2006, 29(3): 52-59
[14]于玉斌, 姚秀萍. 对华北一次特大台风暴雨过程的位涡诊断分析[J]. 高原气象, 2000, 19（1）: 111-120
[15]宇如聪, 曾庆存, 彭贵康, 等. “雅安天漏”研究II: 数值预报实验[J]. 大气科学, 1994, 18（6）: 535-551
[16]宇如聪, 徐幼平. AREM及其对2003年汛期降水的模拟[J]. 气象学报, 2004, 62(6): 715-723
[17]Yu Rucong. A two-step shape-preserving advection scheme[J]. Adv Atmos Sci, 1994, 11(4): 479-490
[18]Yu Rucong. Application of a Shape-preserving advection scheme to the moisture equation in an e-grid regional forecast model[J]. Adv Atmos Sci, 1995, 12(1): 13-19
[19]Betts A K. A new convective adjustment scheme, Part I: Observational and theoretical basis[J]. Quart J Roy Meteor Soc, 1986, 112: 677-691
[20]Xu Y P, D Q Xia, Y Y Qian. The water-bearing numerical model and its operational forecasting experiments Part II: the operational forecasting experiments[J]. Adv Atmos Sci, 1998, 15(3): 321-336
[21]Holtslag A A M, B A Boville. Local versus nonlocal boundary-layer diffusion in a global climate model[J]. J Climate, 1993, 6: 1825-1842
[22]Berjamin S O, N L Seaman. A simple scheme for objective analysis in curved flow[J]. Mon Wea Rev, 1985, 113: 1184-1198
[23]Dickinson R E A. Henderson-Sellers, P J Kennedy. Biosphere-atmosphere transfer scheme (BATS) version le as coupled to the NCAR community climate model[R]. NCAR Tech. Note. NCAR/TN-387+STR, 72
[24]丁一汇. 高等天气学[M]. 北京: 气象出版社, 1991
[25]丁一汇. 天气动力学中的诊断分析方法[M]. 北京: 科学出版社, 1989: 293
[26]丁一汇, 王笑芳. 1983年长江中游梅雨期的热源和热汇分析[J]. 热带气象学报, 1988, 4（2）: 134-145
[27]李昀英, 宇如聪, 傅云飞, 等. 一次热对流降水成因的分析和模拟[J]. 气象学报, 2008, 66（2）: 190-202
[28]叶成志, 欧阳里程, 李象玉, 等. GRAPES中尺度模式对2005年长江流域重大灾害性降水天气过程预报性能的检验分析[J]. 热带气象学报, 2006, 22(4): 393-399
[29]叶成志, 潘志祥, 程锐, 等. 强台风“云娜”登陆过程的研究[J]. 气象学报, 2007, 65(2): 208-228
[30]陶诗言. 中国之暴雨[M]. 北京: 科学出版社, 1980
[31]许美玲, 段旭, 张秀年. 登陆孟湾风暴结构演变特征数值模拟研究[J]. 高原气象, 2006, 25（6）: 1139-1146
[32]Wernli H C, Davies. A Lagrangian-based analysis of extratropical cyclones.Ⅰ: The method and some applications[J]. Quart J Roy Meteor Soc, 1997, 123: 467-489
[33]马京津, 高晓清. 华北地区夏季平均水汽输送通量和轨迹的分析[J]. 高原气象, 2006, 25（5）: 894-898
[34]叶成志, 李昀英, 潘志祥. “碧利斯”登陆后造成的湘东南特大致洪暴雨数值模拟分析[C]. 2006年灾害性天气预报技术高层研讨会会议文集. 2006: 26-35
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