4.7 Article

Evaluation of Satellite-Based Soil Moisture Products over Four Different Continental In-Situ Measurements

期刊

REMOTE SENSING
卷 10, 期 7, 页码 -

出版社

MDPI
DOI: 10.3390/rs10071161

关键词

satellite-based soil moisture; in-situ measurements; AMSR; SMOS; ECV; evaluation

资金

  1. Strategic Priority Research Program of the Chinese Academy of Sciences [XDA19020304]
  2. Geographic Resources and Ecology Knowledge Service System of China Knowledge Center for Engineering Sciences and Technology [CKCEST-2015-1-4]
  3. National Special Program on Basic Science and Technology Research of China [2013FY110900]
  4. National Data Sharing Infrastructure of Earth System Science

向作者/读者索取更多资源

Global, near-real-time satellite-based soil moisture (SM) datasets have been developed over recent decades. However, there has been a lack of comparison among different passing times, retrieving algorithms, and sensors between SM products over various regions. In this study, we assessed seven types of SM products (AMSR_A, AMSR_D, ECV_A, ECV_C, ECV_P, SMOS_A, and SMOS_D) over four different continental in-situ networks in North America, the Tibetan Plateau, Western Europe, and Southeastern Australia. Bias, R, root mean square error (RMSE), unbiased root mean square difference (ubRMSD), anomalies, and anomalies R were calculated to explore the agreement between satellite-based SM and in-situ measurements. Taylor diagrams were drawn for an inter-comparison. The results showed that (1) ECV_C was superior both in characterizing the SM temporal variation tendency and absolute value, while ECV_A produced numerous abnormal values over all validation regions. ECV_P was able to basically express the SM variation tendency, except for a few overestimations and underestimations. (2) The ascending data (AMSR_A, SMOS_A) generally outperformed the corresponding descending data (AMSR_D, SMOS_D). (3) AMSR exceeded SMOS in terms of the coefficient of correlation. (4) The validation result of SMOS_D over the NAN and OZN networks was unsatisfactory, with a rather poor correlation for both original data and anomalies.

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