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农牧交错带陆面过程的数值模拟研究
引用本文:赵海英,郭振海,张宏昇,何金海.农牧交错带陆面过程的数值模拟研究[J].气候与环境研究,2006,11(4):535-545.
作者姓名:赵海英  郭振海  张宏昇  何金海
作者单位:1. 南京信息工程大学大气科学系,南京,210044;中国科学院大气物理研究所大气科学和地球流体力学数值模拟国家重点实验室,北京,100029;山西省气象台,太原,030006
2. 中国科学院大气物理研究所大气科学和地球流体力学数值模拟国家重点实验室,北京,100029
3. 北京大学物理学院大气科学系,北京,100871
4. 南京信息工程大学大气科学系,南京,210044
基金项目:中国科学院知识创新工程重要方向项目KZCX3-SW-218
摘    要:利用CLM(Common Land Model)模式对我国内蒙古奈曼旗农牧交错带沙漠和农田两种不同典型下垫面的陆面过程进行了数值模拟试验,并与外场试验观测结果进行了对比分析。结果表明:无论是沙漠还是农田试验,CLM都能够较好地模拟其辐射通量和土壤中的热传导特征,CLM的模拟结果能够真实地再现试验期间土壤热传导过程对天气过程的响应。相比而言,模式对沙漠地区长波辐射通量和干燥时期短波辐射通量的模拟结果好于农田,其原因可能是因为农田下垫面植被及土壤特征较沙漠复杂,有着很大的不确定性,造成了农田地表反照率和温度模拟的偏差。而对农田热传导的模拟结果好于沙漠,反映了CLM对含水量较大、持水力较强的农田下垫面的热传导模拟能力较好,而对含水量较小、持水力较弱的沙漠下垫面的热传导模拟能力相对较差。

关 键 词:陆面过程  CLM模式  农牧交错带  热传导
文章编号:1006-9585(2006)04-0535-11
收稿时间:06 6 2005 12:00AM
修稿时间:04 19 2006 12:00AM

Numerical Simulation Research of Land Surface Process in the Region between Cropland and Pasture
ZHAO Hai-Ying,GUO Zhen-Hai,ZHANG Hong-Sheng and HE Jin-Hai.Numerical Simulation Research of Land Surface Process in the Region between Cropland and Pasture[J].Climatic and Environmental Research,2006,11(4):535-545.
Authors:ZHAO Hai-Ying  GUO Zhen-Hai  ZHANG Hong-Sheng and HE Jin-Hai
Institution:1. Department of Atmospheric Science, Nanjing University of Information Science and Technology, Nanjing 210044 ;2. State Key Laboratory of Numerical Modeling for Atmospheric Sciences and Geophysical Fluid Dynamics, Institute of Atmospheric Physics, Chinese Academy of Science, Beijing 100029; 3. Department of Atmospheric Science, College of Physics, Peking University, Beijing 100871; 4. Weather Forecast Station of Shanxi Province, Taiyuan 030006
Abstract:In this paper,CLM(common land model) is introduced and numerical simulation test is carried out in desert and cropland respectively,and comparing analysis with observational data of corresponding sites is also made in the region between cropland and pasture in naiman of neimeng province in China.The results of this test show that CLM can effectively simulate the characteristics of radiation flux and thermal conduction of soil in both desert and cropland tests.Furthermore,the simulation of CLM can realistically reproduce the response of thermal conduction in soil to weather process which happened during the test period.But in comparing,as for the simulation of longwave radiation flux in whole test period and shortwave radiation flux in dry period,the result of desert test is better than that of the cropland test,because vegetation and soil feature of cropland is more complicated than those of desert,and to specify them exactly is unpractical,which cause the simulative difference of albedo and land surface temperature in cropland test.But for the simulation of thermal conduction,the result of cropland test is better.This indicate that CLM has a better thermal conduction simulating ability to such land surface as cropland which has big water content and is good at maintain water while has a worse ability to those dry land surface as desert.
Keywords:land surface process  CLM model  region between cropland and pasture  thermal conduction
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