Customization of regional climate model (RegCM4) over Indian region

被引:32
|
作者
Nayak, S. [1 ]
Mandal, M. [1 ]
Maity, S. [1 ]
机构
[1] Indian Inst Technol Kharagpur, Ctr Oceans Rivers Atmosphere & Land Sci, Kharagpur 721302, W Bengal, India
关键词
CONVECTIVE PARAMETERIZATION SCHEMES; PART I; MONSOON PRECIPITATION; CUMULUS CONVECTION; AFRICAN MONSOON; EAST-ASIA; SIMULATION; SENSITIVITY; TEMPERATURE; CHINA;
D O I
10.1007/s00704-015-1630-8
中图分类号
P4 [大气科学(气象学)];
学科分类号
0706 ; 070601 ;
摘要
The regional climate model (RegCM4) is customized for 10-year climate simulation over Indian region through sensitivity studies on cumulus convection and land surface parameterization schemes. The model is configured over 30A degrees E-120A degrees E and 15A degrees S-45A degrees N at 30-km horizontal resolution with 23 vertical levels. Six 10-year (1991-2000) simulations are conducted with the combinations of two land surface schemes (BATS, CLM3.5) and three cumulus convection schemes (Kuo, Grell, MIT). The simulated annual and seasonal climatology of surface temperature and precipitation are compared with CRU observations. The interannual variability of these two parameters is also analyzed. The results indicate that the model simulated climatology is sensitive to the convection as well as land surface parameterization. The analysis of surface temperature (precipitation) climatology indicates that the model with CLM produces warmer (dryer) climatology, particularly over India. The warmer (dryer) climatology is due to the higher sensible heat flux (lower evapotranspiration) in CLM. The model with MIT convection scheme simulated wetter and warmer climatology (higher precipitation and temperature) with smaller Bowen ratio over southern India compared to that with the Grell and Kuo schemes. This indicates that a land surface scheme produces warmer but drier climatology with sensible heating contributing to warming where as a convection scheme warmer but wetter climatology with latent heat contributing to warming. The climatology of surface temperature over India is better simulated by the model with BATS land surface model in combination with MIT convection scheme while the precipitation climatology is better simulated with BATS land surface model in combination with Grell convection scheme. Overall, the modeling system with the combination of Grell convection and BATS land surface scheme provides better climate simulation over the Indian region.
引用
收藏
页码:153 / 168
页数:16
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