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《Desert and Oasis Meteorology》 2018-06
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Applicability of Different Parameterization Schemes of Land Surface Model Noah-MP in Desert Areas

LI Huoqing;ALI Mamtimin;LIU Yongqiang;JU Chenxiang;Institute of Desert Meteorology,CMA, Taklimakan Desert Meteorology Field Experiment Station of CMA;College of Resource and Environmental Sciences,Xinjiang University;  
In order to study the optimal parameterization scheme of the land surface model Noah-MP in the desert underlying surface, we designed three sets of combinatorial experiments of different parameterization schemes according to the characteristics of the desert environment, which based on the observation data over the Taklimakan Desert Meteorology Field Experiment Station of CMA, and then get the optimal combination of parameterization schemes. The results show that the 3rd experiment has the best simulation effect on soil temperature of 10 cm, the main reason is that the sensible heat exchange coefficient Chen97 and radiation transfer scheme the entire grid cell two-stream approximation(gap=0) are in line with the environment characteristics of the desert. Because of the soil information could not reflected in the model, all of experiments have poor simulation effect of soil moisture, the 2nd experiment chooses soil moisture factor for stomatal resistance scheme CLM which considerated the influence of soil evaporation, so that has better correlation. As for the sensible heat flux, the 1st and 2nd experiment overestimated at the peak, the second set of simulation are significantly underestimated after precipitation especially, the 3rd experiment has the best simulation effect, the mainly reason is that selection of scheme for sensible heat exchange coefficient Chen97,which described the Ch variation characteristics more realistically. Due to the desert soil moisture is extremely low, the latent heat flux has the worst simulation effect among the four characteristic variables, which actual infiltration of soil water is less than observed precipitation, which cannot accurately calculate soil evaporation and vegetation evapotranspiration because that desert has no vegetation and plant roots. Based on the statistical and the Taylor diagram show that the 3rd set of simulations has the best performance in the desert area.
【Fund】: 中亚大气科学基金(CAAS201811 CASS201711);; 国家自然科学基(41801019 41875023 41675011 41265002 41605008);; 中央级公益性科研院所基本科研业务费专项(IDM2017001)共同资助
【CateGory Index】: P456
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