Arid
DOI10.1016/j.geoderma.2020.114583
Evaluation of reanalysis soil temperature and soil moisture products in permafrost regions on the Qinghai-Tibetan Plateau
Yang, Shuhua; Li, Ren; Wu, Tonghua; Hu, Guojie; Xiao, Yao; Du, Yizhen; Zhu, Xiaofan; Ni, Jie; Ma, Junjie; Zhang, Yuxin; Shi, Jianzong; Qiao, Yongping
通讯作者Li, R
来源期刊GEODERMA
ISSN0016-7061
EISSN1872-6259
出版年2020
卷号377
英文摘要Long-term and large-scale reanalysis products of soil temperature and soil moisture are very important for understanding the hydrothermal regime in permafrost regions. However, it is necessary to evaluate the reliability of these products before using them. In this study, five in situ observed sites with different land cover types were collected to evaluate the performance of soil temperature and soil moisture in four reanalysis products from 2013 to 2014 in permafrost regions on the Qinghai-Tibetan Plateau (QTP). The four reanalysis products included three widely used products derived from the Climate Forecast System Reanalysis version 2 (CFSv2), the European Centre for Medium-Range Weather Forecasts (ECMWF) interim reanalysis (ERA-Interim), and the Noah model driven by the Global Land Data Assimilation System (GLDAS-Noah), as well as a latest reanalysis product from the fifth-generation reanalysis product by the ECMWF (ERAS). The results showed that all of these products could capture temporal dynamics of soil temperature (R > 0.8) and soil moisture (R > 0.4) well. However, soil temperature was underestimated, and soil moisture was overestimated during the thawing period. The investigated results showed, those errors may mainly be caused by soil properties and forcing data. In addition, the mismatch of spatial scales between the reanalysis products and in situ observed sites, and parameterization schemes in the land surface models, such as soil thermal and hydraulic conductivity schemes, may also contributed partly causes of simulation errors. Overall, the statistical results showed that GLDAS-Noah product ranked at the top of the four products in simulating soil temperature, especially in the alpine desert, alpine swamp and alpine grassy meadow. And ERA-Interim product was superior to the other products in simulating soil moisture in permafrost regions on the QTP, especially in the alpine desert and alpine meadow. Additionally, we found that ERAS product was better than ERA-Interim product in simulating soil temperature, especially in topsoil, but it did not show superior performance in simulating soil moisture in permafrost regions of the QTP. This may be related to the different land surface models and soil texture between the two products.
英文关键词Soil temperature Soil moisture Reanalysis product Permafrost Qinghai-Tibetan Plateau
类型Article
语种英语
收录类别SCI-E
WOS记录号WOS:000560363900011
WOS关键词WATER STORAGE ; CLIMATE-CHANGE ; FROZEN SOIL ; IMPACTS ; SIMULATIONS ; PERFORMANCE ; CARBON ; NCEP ; AIR
WOS类目Soil Science
WOS研究方向Agriculture
资源类型期刊论文
条目标识符http://119.78.100.177/qdio/handle/2XILL650/325660
作者单位[Yang, Shuhua; Li, Ren; Wu, Tonghua; Hu, Guojie; Xiao, Yao; Du, Yizhen; Zhu, Xiaofan; Ni, Jie; Ma, Junjie; Zhang, Yuxin; Shi, Jianzong; Qiao, Yongping] Chinese Acad Sci, Northwest Inst Ecoenvironm & Resources, State Key Lab Cryospher Sci, Cryosphere Res Stn Qinghai Tibetan Plateau, Lanzhou 730000, Peoples R China; [Yang, Shuhua; Du, Yizhen; Ni, Jie; Ma, Junjie; Zhang, Yuxin] Univ Chinese Acad Sci, Beijing 100049, Peoples R China
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Yang, Shuhua,Li, Ren,Wu, Tonghua,et al. Evaluation of reanalysis soil temperature and soil moisture products in permafrost regions on the Qinghai-Tibetan Plateau[J],2020,377.
APA Yang, Shuhua.,Li, Ren.,Wu, Tonghua.,Hu, Guojie.,Xiao, Yao.,...&Qiao, Yongping.(2020).Evaluation of reanalysis soil temperature and soil moisture products in permafrost regions on the Qinghai-Tibetan Plateau.GEODERMA,377.
MLA Yang, Shuhua,et al."Evaluation of reanalysis soil temperature and soil moisture products in permafrost regions on the Qinghai-Tibetan Plateau".GEODERMA 377(2020).
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