中国科学院机构知识库网格
Chinese Academy of Sciences Institutional Repositories Grid
Validation of the global land data assimilation system based on measurements of soil temperature profiles

文献类型:期刊论文

作者Wang, L; Qi, J (Qi, Jia)3; Huang, JB (Huang, Jianbin)4,5; Li, XP; Wang, L (Wang, Lei)2,3; Li, XP (Li, Xiuping)3; Chen, YY (Chen, Yingying)2,3; Yang, K (Yang, Kun)2,3; Chen, DL (Chen, Deliang)1; Zhou, J (Zhou, Jing)3
刊名AGRICULTURAL AND FOREST METEOROLOGY
出版日期2016
卷号218期号:0页码:288-297
关键词Surface Model Eta-model Carbon-dioxide Climate Models Moisture Satellite Water Products Weather Fluxes
DOI10.1016/j.agrformet.2016.01.003
文献子类Article
英文摘要Soil temperature is a key parameter in the soil-vegetation-atmosphere system. It plays an important role in the land surface water and energy cycles, and has a major influence on vegetation growth and other hydrological aspects. We evaluated the accuracy of the soil temperature profiles from the Global Land Data Assimilation System (GLDAS) using nine observational networks across the world and aimed to find a reliable global soil temperature profile dataset for future hydrological and ecological studies. In general, the soil temperature profile data generated by the Noah model driven by the GLDAS forcing data (GLDAS_Noah10 and GLDAS_Noah10_v2) were found to have high skills in terms of daily, monthly, and mean seasonal variations, indicated by smaller bias and root-mean-square-error (RMSE) (both <3 degrees C) and correlation coefficients larger than 0.90. Conversely, the Community Land Model (CLM) results (GLDAS_CLM10) generally showed larger bias and RMSE (both >4 degrees C). Further analysis showed that the overestimation by GLDAS_CLM10 was mainly caused by overestimation of the ground heat flux, determined by the thermal conductivity parameterization scheme, whereas the underestimation by GLDAS_Noah10 was due to underestimation of downward longwave radiation from the forcing data. Thus, more accurate forcing data should be required for the Noah model and an improved thermal parameterization scheme should be developed for the CLM. These approaches will improve the accuracy of simulated soil temperatures. To our knowledge, it is the first study to evaluate the GLDAS soil temperatures with comprehensive in situ observations across the world, and has a potential to facilitate an overall improvement of the GLDAS products (not only soil temperatures but also the related energy and water fluxes) as well as a refinement of the land surface parameterization used in GLDAS. (C) 2016 Elsevier B.V. All rights reserved.
学科主题自然地理学
语种英语
WOS记录号WOS:000370905100028
源URL[http://ir.itpcas.ac.cn/handle/131C11/7734]  
专题青藏高原研究所_图书馆
通讯作者Wang, L; Li, XP
作者单位1.Univ Gothenburg, Dept Earth Sci, Gothenburg, Sweden
2.Chinese Acad Sci, Ctr Excellence Tibetan Plateau Earth Sci, Beijing, Peoples R China
3.Chinese Acad Sci, Inst Tibetan Plateau Res, Key Lab Tibetan Environm Changes & Land Surface P, Bldg 3,Courtyard 16,Lin Cui Rd, Beijing, Peoples R China
4.Tsinghua Univ, Minist Educ, Key Lab Earth Syst Modeling, Beijing 100084, Peoples R China
5.Tsinghua Univ, Ctr Earth Syst Sci, Beijing 100084, Peoples R China
推荐引用方式
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Wang, L,Qi, J ,Huang, JB ,et al. Validation of the global land data assimilation system based on measurements of soil temperature profiles[J]. AGRICULTURAL AND FOREST METEOROLOGY,2016,218(0):288-297.
APA Wang, L.,Qi, J .,Huang, JB .,Li, XP.,Wang, L .,...&Liu, WB .(2016).Validation of the global land data assimilation system based on measurements of soil temperature profiles.AGRICULTURAL AND FOREST METEOROLOGY,218(0),288-297.
MLA Wang, L,et al."Validation of the global land data assimilation system based on measurements of soil temperature profiles".AGRICULTURAL AND FOREST METEOROLOGY 218.0(2016):288-297.

入库方式: OAI收割

来源:青藏高原研究所

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