A Regional Model Simulation of the 1991 Severe Precipitation Event over the Yangtze–Huai River Valley. Part I: Precipitation and Circulation Statistics

Abstract The summer Mei-yu event over eastern China, which is strongly influenced by large-scale circulation, is an important aspect of East Asian climate; for example, the Mei-yu frequently brings heavy precipitation to the Yangtze–Huai River valley (YHRV). Both observations and a regional model were used to study the Mei-yu front and its relation to large-scale circulation during the summer of 1991 when severe floods occurred over YHRV. This study has two parts: the first part, presented here, analyzes the association between heavy Mei-yu precipitation and relevant large-scale circulation, while the second part, documented by W. Gong and W.-C. Wang, examines the model biases associated with the treatment of lateral boundary conditions (the objective analyses and coupling schemes) used as the driving fields for the regional model. Observations indicate that the Mei-yu season in 1991 spans 18 May–14 July, making it the longest Mei-yu period during the last 40 yr. The heavy precipitation over YHRV is found...

[1]  Ka-Ming Lau,et al.  The Monsoon of East Asia and its Global Associations—A Survey , 1984 .

[2]  Wei‐Chyung Wang,et al.  Interannual variability of regional climate and its change due to the greenhouse effect , 1995 .

[3]  S. Tao,et al.  A review of recent research on the East Asian summer monsoon in China , 1987 .

[4]  Xin-Zhong Liang,et al.  A Regional Climate Model Study of the Scale Dependence of Cloud-Radiation Interactions. , 1996 .

[5]  G. Grell,et al.  A description of the fifth-generation Penn State/NCAR Mesoscale Model (MM5) , 1994 .

[6]  J. Dudhia Numerical Study of Convection Observed during the Winter Monsoon Experiment Using a Mesoscale Two-Dimensional Model , 1989 .

[7]  Wei-Chyung Wang,et al.  A Regional Model Simulation of the 1991 Severe Precipitation Event over the Yangtze–Huai River Valley. Part II: Model Bias , 2000 .

[8]  H. Davies,et al.  A lateral boundary formulation for multi-level prediction models. [numerical weather forecasting , 1976 .

[9]  Jun Li,et al.  Large-Scale Conditions Favorable for the Development of Heavy Rainfall during TAMEX IOP 3 , 1995 .

[10]  Wei‐Chyung Wang,et al.  A GCM Study of the Climatic Effect of 1979–1992 Ozone Trend , 1995 .

[11]  G. T. Chen,et al.  Study of low-level jet and extremely heavy rainfall over northern Taiwan in the Mei-Yu season , 1988 .

[12]  Da‐Lin Zhang,et al.  A High-Resolution Model of the Planetary Boundary Layer—Sensitivity Tests and Comparisons with SESAME-79 Data , 1982 .

[13]  Analysis of the East Asian Monsoon during Early Summer of 1979 Structure of the Baiu Front and its R , 1993 .

[14]  Gerald L. Potter,et al.  Simulation of the Northern Summer Monsoon in the ECMWF Model: Sensitivity to Horizontal Resolution , 1994 .

[15]  Shaowu Wang,et al.  A Comparison between Observed and GCM-Simulated Summer Monsoon Characteristics over China , 1995 .

[16]  D. Pollard,et al.  A Global Climate Model (GENESIS) with a Land-Surface Transfer Scheme (LSX). Part I: Present Climate Simulation. , 1995 .

[17]  Roni Avissar,et al.  Simulation with the regional climate model RegCM2 of extremely anomalous precipitation during the 1991 east Asian flood: An evaluation study , 1996 .

[18]  Ching-Sen Chen,et al.  A Study of a Mountain-generated Precipitation System in Northern Taiwan during TAMEX IOP 8 , 1991 .

[19]  J. Dudhia,et al.  The evolution of the East Asia summer monsoon in June 1994: Numerical simulations , 1998 .

[20]  Y. Kuo,et al.  Description of the Penn State/NCAR Mesoscale Model: Version 4 (MM4) , 1987 .

[21]  Steven J. Nieman,et al.  The Multiyear Surface Climatology of a Regional Atmospheric Model over the Western United States , 1993 .