Effects of crop growth and development on regional climate: a case study over East Asian monsoon area

被引:27
作者
Chen, Feng [1 ,2 ]
Xie, Zhenghui [1 ]
机构
[1] Chinese Acad Sci, LASG, Inst Atmospher Phys, Beijing 100029, Peoples R China
[2] Zhejiang Inst Meteorol Sci, Hangzhou 310017, Zhejiang, Peoples R China
基金
中国国家自然科学基金;
关键词
Crop growth and development; Regional climate; East Asian monsoon area; 3-DIMENSIONAL ATMOSPHERIC SIMULATIONS; SEASONAL PLANT-GROWTH; SURFACE FLUXES; RADIATIVE-TRANSFER; MODEL REGCM2; PRECIPITATION; CHINA; PREDICTION; VEGETATION; EVENTS;
D O I
10.1007/s00382-011-1125-y
中图分类号
P4 [大气科学(气象学)];
学科分类号
0706 ; 070601 ;
摘要
In this study, the CERES phenological growth and development functions were implemented into the regional climate model, RegCM3 to give a model denoted as RegCM3_CERES. This model was used to represent interactions between regional climate and crop growth processes. The effects of crop growth and development processes on regional climate were then studied based on two 20-year simulations over the East Asian monsoon area conducted using the original regional climate model RegCM3, and the coupled RegCM3_CERES model. The numerical experiments revealed that incorporating the crop growth and development processes into the regional climate model reduced the root mean squared error of the simulated precipitation by 2.2-10.7% over north China, and the simulated temperature by 5.5-30.9% over the monsoon region in eastern China. Comparison of the simulated results obtained using RegCM3_CERES and RegCM3 showed that the most significant changes associated with crop modeling were the changes in leaf area index which in turn modify the aspects of surface energy and water partitions and lead to moderate changes in surface temperature and, to some extent, rainfall. Further analysis revealed that a robust representation of seasonal changes in plant growth and developmental processes in the regional climate model changed the surface heat and moisture fluxes by modifying the vegetation characteristics, and that these differences in simulated surface fluxes resulted in different structures of the boundary layer and ultimately affected the convection. The variations in leaf area index and fractional vegetation cover changed the distribution of evapotranspiration and heat fluxes, which could potentially lead to anomalies in geopotential height, and consequently influenced the overlying atmospheric circulation. These changes would result in redistribution of the water and energy through advection. Nevertheless, there are significant uncertainties in modeling how monsoon dynamics responds to crop modeling and more research is needed.
引用
收藏
页码:2291 / 2305
页数:15
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