South China Heavy Rainfall Experiments (SCHeREX)

被引:36
作者
Zhang, Renhe [1 ]
Ni, Yongqi [1 ]
Liu, Liping [1 ]
Luo, Yali [1 ]
Wang, Yehong [2 ]
机构
[1] Chinese Acad Meteorol Sci, State Key Lab Severe Weather LaSW, 46 Zhong Guan Cun S Ave, Beijing 100081, Peoples R China
[2] CMA, Inst Heavy Rain, Wuhan, Peoples R China
基金
中国国家自然科学基金;
关键词
D O I
10.2151/jmsj.2011-A10
中图分类号
P4 [大气科学(气象学)];
学科分类号
0706 ; 070601 ;
摘要
The South China Heavy Rainfall Experiments (SCHeREX) was staged during 2008 and 2009 in the southern part of China by the Chinese Academy of Meteorological Sciences under the support of the Chinese Ministry of Science and Technology and China Meteorological Administration. SCHeREX aims at obtaining abundant observational datasets at the meso-beta scale, better understanding of the structure and evolution of heavy precipitation systems in south China, exploring establishment of an operational platform for heavy rainfall monitoring and prediction, and improving the ability of heavy rainfall monitoring and prediction. Four zones were selected in SCHeREX, namely, the southern China, the middle reaches of the Yangtze River valley, the Huai River valley, and the lower reaches of the Yangtze River valley. The observation phases were May 1 June 10 in the southern China zone and June 10 July 20 in the other three zones. The efforts have led to the establishment of the meso-scale observing networks with enhanced capacity to observe precipitation systems at the meso-beta scale level. The collected data have been utilized in meso-scale reanalysis not only to reveal the fine structures of the precipitation systems but also to provide better initial conditions for mesa-scale numerical models to make short-term forecasts. Assimilation of the dropsonde data has improved the analysis of the locations and intensities of typhoons Goni and Morakot. With the real-time field data being part of the forecast system, the experiments have allowed more efficient interactions between the observing system and the forecast system and thus improve the performance of meso-scale heavy rainfall forecasts.
引用
收藏
页码:153 / 166
页数:14
相关论文
共 22 条
  • [1] ALBERS SCJ, 1996, ANALYSIS, V11, P287
  • [2] [陈子通 Chen Zitong], 2010, [热带气象学报, Journal of Tropical Meteorology], V26, P49
  • [3] CHOI YJ, 2006, 2 KOR JAP CHIN JOINT
  • [4] Ding Y., 1994, MONSOON CHINA
  • [5] Ding YH, 2004, ADV ATMOS SCI, V21, P343
  • [6] Ding YH, 2001, J METEOROL SOC JPN, V79, P277
  • [7] Reason for the failure of the simulation of heavy rainfall during X-BAIU-01 - Importance of a vertical profile of water vapor for numerical simulations
    Kato, T
    Yoshizaki, M
    Bessho, K
    Inoue, T
    Sato, Y
    [J]. JOURNAL OF THE METEOROLOGICAL SOCIETY OF JAPAN, 2003, 81 (05) : 993 - 1013
  • [8] KUO YH, 1990, B AM METEOROL SOC, V71, P488, DOI 10.1175/1520-0477(1990)071<0488:TTAMEA>2.0.CO
  • [9] 2
  • [10] Modeling convective-stratiform precipitation processes on a Mei-Yu front with the Weather Research and Forecasting model: Comparison with observations and sensitivity to cloud microphysics parameterizations
    Luo, Yali
    Wang, Yanjie
    Wang, Hongyan
    Zheng, Yongjun
    Morrison, Hugh
    [J]. JOURNAL OF GEOPHYSICAL RESEARCH-ATMOSPHERES, 2010, 115