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DOI10.1029/2021JD035177
Modification and Comparison of Thermal and Hydrological Parameterization Schemes for Different Underlying Surfaces on the Tibetan Plateau in the Warm Season
Yuan, Yuan; Ma, Yaoming; Zuo, Hongchao; Yang, Chenyi; Yuan, Ling; Chen, Jinlei
通讯作者Ma, YM (通讯作者),Lanzhou Univ, Coll Atmospher Sci, Lanzhou, Peoples R China. ; Ma, YM (通讯作者),Chinese Acad Sci, Inst Tibetan Plateau Res, Key Lab Tibetan Environm Changes & Lar Surface Pr, Beijing, Peoples R China. ; Ma, YM (通讯作者),Univ Chinese Acad Sci, Beijing, Peoples R China. ; Ma, YM (通讯作者),Chinese Acad Sci, CAS Ctr Excellence Tibetan Plateau Earth Sci, Beijing, Peoples R China.
发表日期2021
ISSN2169-897X
EISSN2169-8996
卷号126期号:22
英文摘要In this paper, three parameterization schemes, one considering gravel influence (test1), one considering organic carbon influence (test2), and one comprehensively considering gravel and organic carbon influence (test3), were set up to modify different typical underlying surfaces of the Tibetan Plateau (TP). In addition, their soil thermal properties and hydraulic property variations were discussed. Additionally, discussing the key thermal and hydraulic parameters affected the performance of different schemes from the perspective of observation data in the TP to improve the simulation ability of soil temperature and soil moisture in the plateau areas. Compared the original Community Land Model (CLM) scheme, test1 resulted in higher soil temperature and lower soil moisture, while test2 had lower soil temperature and higher soil moisture. The key thermal and hydraulic parameters are the changes in the saturated thermal conductivity and the thermal conductivity of dry soil and the variations of the porosity and exponent B, respectively. The test3 scheme was the same as test2 for the modified changes of thermal properties, except that the proportion of change was slightly different. In terms of soil thermal properties, test2 and test3 were better at 0-20 cm depth, while test1 and test3 were better for the deeper (40 cm) simulation. Regarding hydraulic properties, the test1 and test3 schemes performed better on the Gobi and alpine meadows at 20-40 cm depth, while the original CLM scheme and test2 performed better on the underlying grassland surface. Test3 was better at balancing the relationship between the thermal and hydraulic parameters and could be used for the further research on the entire plateau area.
关键词SOILCIRCULATIONGRAVELMODEL
英文关键词Tibetan Plateau; parameterization scheme; thermal properties; hydraulic properties
语种英语
WOS研究方向Meteorology & Atmospheric Sciences
WOS类目Meteorology & Atmospheric Sciences
WOS记录号WOS:000723100300006
来源期刊JOURNAL OF GEOPHYSICAL RESEARCH-ATMOSPHERES
来源机构中国科学院西北生态环境资源研究院
文献类型期刊论文
条目标识符http://gcip.llas.ac.cn/handle/2XKMVOVA/254877
作者单位[Yuan, Yuan; Ma, Yaoming; Zuo, Hongchao; Yang, Chenyi] Lanzhou Univ, Coll Atmospher Sci, Lanzhou, Peoples R China; [Ma, Yaoming; Yuan, Ling] Chinese Acad Sci, Inst Tibetan Plateau Res, Key Lab Tibetan Environm Changes & Lar Surface Pr, Beijing, Peoples R China; [Ma, Yaoming; Yuan, Ling] Univ Chinese Acad Sci, Beijing, Peoples R China; [Ma, Yaoming] Chinese Acad Sci, CAS Ctr Excellence Tibetan Plateau Earth Sci, Beijing, Peoples R China; [Chen, Jinlei] Chinese Acad Sci, Northwest Inst Ecoenvironm & Resources, State Key Lab Cryosphere Sci, Lanzhou, Peoples R China
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GB/T 7714
Yuan, Yuan,Ma, Yaoming,Zuo, Hongchao,et al. Modification and Comparison of Thermal and Hydrological Parameterization Schemes for Different Underlying Surfaces on the Tibetan Plateau in the Warm Season[J]. 中国科学院西北生态环境资源研究院,2021,126(22).
APA Yuan, Yuan,Ma, Yaoming,Zuo, Hongchao,Yang, Chenyi,Yuan, Ling,&Chen, Jinlei.(2021).Modification and Comparison of Thermal and Hydrological Parameterization Schemes for Different Underlying Surfaces on the Tibetan Plateau in the Warm Season.JOURNAL OF GEOPHYSICAL RESEARCH-ATMOSPHERES,126(22).
MLA Yuan, Yuan,et al."Modification and Comparison of Thermal and Hydrological Parameterization Schemes for Different Underlying Surfaces on the Tibetan Plateau in the Warm Season".JOURNAL OF GEOPHYSICAL RESEARCH-ATMOSPHERES 126.22(2021).
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