中国科学院机构知识库网格
Chinese Academy of Sciences Institutional Repositories Grid
Surface Soil Moisture Drydown over the Tibetan Plateau from SMAP: Consistency with In Situ Observations, Spatial Patterns and Controls

文献类型:期刊论文

作者Dong, Shiyu1,2; Zhu, Zhongli2; Zhang, Jinsong2; Liu, Ziqi3; Wu, Qingxia2
刊名REMOTE SENSING
出版日期2026-03-06
卷号18期号:5页码:814
关键词soil moisture in situ networks drydown timescale SMAP Tibetan plateau
DOI10.3390/rs18050814
产权排序2
文献子类Article
英文摘要Highlights What are the main findings? SMAP satellite products systematically yield shorter soil moisture drydown timescales () compared to in situ observations. tau The drydown timescale exhibits a distinct southeast-to-northwest gradient across the Tibetan Plateau, primarily driven by elevation, soil sand fraction, and vegetation. What are the implications of the main findings? Discrepancies between satellite and ground estimates highlight the critical impact of effective sensing depth and spatial representativeness on soil memory characterization. Accounting for sensing-depth limitations and representativeness is essential for unbiased satellite-based tau applications in drought diagnostics and land-atmosphere coupling.Highlights What are the main findings? SMAP satellite products systematically yield shorter soil moisture drydown timescales () compared to in situ observations. tau The drydown timescale exhibits a distinct southeast-to-northwest gradient across the Tibetan Plateau, primarily driven by elevation, soil sand fraction, and vegetation. What are the implications of the main findings? Discrepancies between satellite and ground estimates highlight the critical impact of effective sensing depth and spatial representativeness on soil memory characterization. Accounting for sensing-depth limitations and representativeness is essential for unbiased satellite-based tau applications in drought diagnostics and land-atmosphere coupling.Abstract Soil moisture (SM) mediates land-atmosphere water and energy exchanges and is therefore central to evapotranspiration, drought evolution, and hydroclimate extremes. The SM drydown timescale (tau), typically derived from exponential decay fits following rainfall or snowmelt rewetting, provides a compact measure of near-surface memory and drying rate. Despite the availability of microwave satellite SM products, their reliability for drydown characterization over the Tibetan Plateau remains uncertain, and systematic evaluations of drydown events and tau against in situ networks are still limited. Here, we integrate five Tibetan Plateau (TP) soil moisture sensor networks with SMAP to (i) assess consistency in drydown event detection and tau estimation across observation systems and (ii) map TP-wide tau patterns and identify dominant controls using SMAP (2016-2025). SMAP-derived tau is generally smaller than in situ tau, indicating a faster drying signal in the satellite product; this may be attributed to differences in effective sensing depth and spatial representativeness between satellite footprints and point measurements. TP SMAP tau exhibits a pronounced southeast-to-northwest decreasing gradient, with the shortest tau over the arid interior. Partial least squares regression identifies elevation, sand fraction, and vegetation conditions as primary drivers of spatial tau variability. This research provides observational constraints for understanding land-surface hydrological processes and land-atmosphere coupling in alpine regions.
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WOS关键词SATELLITE ; TERM
WOS研究方向Environmental Sciences & Ecology ; Geology ; Remote Sensing ; Imaging Science & Photographic Technology
语种英语
WOS记录号WOS:001713936200001
出版者MDPI
源URL[http://ir.igsnrr.ac.cn/handle/311030/221312]  
专题生态系统网络观测与模拟院重点实验室_外文论文
通讯作者Zhu, Zhongli
作者单位1.Chinese Acad Sci, Inst Geog Sci & Nat Resources Res, Key Lab Ecosyst Network Observat & Modeling, Beijing 100101, Peoples R China;
2.Beijing Normal Univ, Fac Geog Sci, State Key Lab Earth Surface Proc & Disaster Risk R, Beijing 100875, Peoples R China;
3.Chinese Acad Meteorol Sci, Beijing 100081, Peoples R China
推荐引用方式
GB/T 7714
Dong, Shiyu,Zhu, Zhongli,Zhang, Jinsong,et al. Surface Soil Moisture Drydown over the Tibetan Plateau from SMAP: Consistency with In Situ Observations, Spatial Patterns and Controls[J]. REMOTE SENSING,2026,18(5):814.
APA Dong, Shiyu,Zhu, Zhongli,Zhang, Jinsong,Liu, Ziqi,&Wu, Qingxia.(2026).Surface Soil Moisture Drydown over the Tibetan Plateau from SMAP: Consistency with In Situ Observations, Spatial Patterns and Controls.REMOTE SENSING,18(5),814.
MLA Dong, Shiyu,et al."Surface Soil Moisture Drydown over the Tibetan Plateau from SMAP: Consistency with In Situ Observations, Spatial Patterns and Controls".REMOTE SENSING 18.5(2026):814.

入库方式: OAI收割

来源:地理科学与资源研究所

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