NUMERICAL EXPERIMENTAL STUDY FOR THE EFFECT OF A BINARY TYPHOON SYSTEM ON THE EXTREME RAINFALL OF TYPHOON MORAKOT (0908)

被引:2
|
作者
Xu, Yinglong [1 ,2 ,3 ]
Lu, Xinyan [3 ]
机构
[1] Chinese Acad Meteorol Sci, Beijing, Peoples R China
[2] Nanjing Univ Informat Sci & Technol, Nanjing, Peoples R China
[3] Natl Meteorol Ctr CMA, 46 Zhongguancun S St, Beijing 100081, Peoples R China
基金
中国国家自然科学基金;
关键词
typhoon Morakot; binary typhoon system; extreme rainfall; numerical simulation;
D O I
10.6057/2014TCRR01.03
中图分类号
P4 [大气科学(气象学)];
学科分类号
0706 ; 070601 ;
摘要
A high-resolution numerical simulation of the extreme rainfall caused by typhoon Morakot (0908) over Taiwan Province, China, was made using the WRF-ARW/NCAR model (Version 3.2), ERA Interim reanalysis data (resolution: 1.5 degrees x1.5 degrees) from the European Centre for Medium-Range Weather Forecasts (ECMWF), and global real-time sea surface temperature analysis data (RTG_SST, 0.5 degrees x0.5 degrees) from NCEP/NOAA. The numerical simulation results showed that the extreme rainfall caused by Morakot over Taiwan was closely related to water vapor transport of the southwesterly flow. However, the effect of a binary typhoon system between Morakot and Severe Tropical Storm Goni (0907) was also an important factor. Goni strengthened the intensity of the southwesterly flow and the water vapor transport to Morakot and resulted in the heavy rainfall increasing over central and southern mountainous areas of Taiwan. Furthermore, the effect of the binary typhoon system increasing the northward component of the track of Morakot, and the typhoon's slow translation to Taiwan, caused the longtime and persistent severe rainfall over southern Taiwan. After removing Goni's circulation in the model initial field, the cumulative precipitation was greatly reduced by 35.78%, 33.03% and 31.5% in the 18-, 6-and 2-km resolution model results, respectively.
引用
收藏
页码:35 / 43
页数:9
相关论文
共 50 条
  • [1] NUMERICAL EXPERIMENTAL STUDY FOR THE EFFECT OF A BINARY TYPHOON SYSTEM ON THE EXTREME RAINFALL OF TYPHOON MORAKOT(0908)
    YINGLONG XU
    XINYAN LU
    Tropical Cyclone Research and Review, 2014, (01) : 35 - 43
  • [2] On the extreme rainfall of Typhoon Morakot (2009)
    Chien, Fang-Ching
    Kuo, Hung-Chi
    JOURNAL OF GEOPHYSICAL RESEARCH-ATMOSPHERES, 2011, 116
  • [3] Lightning Activity in Typhoon Morakot(0908)
    Wen, Ying
    Zhao, Yang
    Kong, Xiangzhen
    2014 INTERNATIONAL CONFERENCE ON LIGHTNING PROTECTION (ICLP), 2014, : 1291 - 1298
  • [4] Extreme Rainfall Mechanisms Exhibited by Typhoon Morakot (2009)
    Huang, Ching-Yuang
    Wong, Chan-Seng
    Yeh, Tien-Chiang
    TERRESTRIAL ATMOSPHERIC AND OCEANIC SCIENCES, 2011, 22 (06): : 613 - 632
  • [5] Monsoon effect simulation on typhoon rainfall potential - Typhoon Morakot (2009)
    Chang, Yi-Ling
    Yeh, Hsi-Chyi
    Liu, Gin-Rong
    Liu, Chian-Yi
    Liu, Chung-Chih
    Lin, Tang-Huang
    TERRESTRIAL ATMOSPHERIC AND OCEANIC SCIENCES, 2017, 28 (01): : 11 - 21
  • [6] CAN THE EXTREME RAINFALL ASSOCIATED WITH TYPHOON MORAKOT (2009) HAPPEN IN HONG KONG?
    Chan, S. T.
    Huang, Yiwu
    TROPICAL CYCLONE RESEARCH AND REVIEW, 2012, 1 (01) : 1 - 15
  • [7] CAN THE EXTREME RAINFALL ASSOCIATED WITH TYPHOON MORAKOT (2009) HAPPEN IN HONG KONG?
    S.T.CHAN
    YIWU HUANG
    Tropical Cyclone Research and Review, 2012, (01) : 1 - 12
  • [8] ON THE RELATIONSHIPS BETWEEN THE UNUSUAL TRACK OF TYPHOON MORAKOT(0908)AND THE UPPER WESTERLY TROUGH
    费建芳
    李波
    黄小刚
    程小平
    Journal of Tropical Meteorology, 2012, 18 (02) : 187 - 194
  • [9] ON THE RELATIONSHIPS BETWEEN THE UNUSUAL TRACK OF TYPHOON MORAKOT (0908) AND THE UPPER WESTERLY TROUGH
    Fei Jian-fang
    Li Bo
    Huang Xiao-gang
    Cheng Xiao-ping
    JOURNAL OF TROPICAL METEOROLOGY, 2012, 18 (02) : 187 - 194
  • [10] How much of Typhoon Morakot's extreme rainfall is attributable to anthropogenic climate change?
    Wang, Chung-Chieh
    Tseng, Li-Shan
    Huang, Chien-Chang
    Lo, Shih-How
    Chen, Cheng-Ta
    Chuang, Pi-Yu
    Su, Nan-Chou
    Tsuboki, K.
    INTERNATIONAL JOURNAL OF CLIMATOLOGY, 2019, 39 (08) : 3454 - 3464