Testing regression equations to derive long-term global soil moisture datasets from passive microwave observations

被引:41
作者
Al-Yaari, A. [1 ]
Wigneron, J. P. [1 ]
Kerr, Y. [2 ]
de Jeu, R. [3 ,4 ]
Rodriguez-Fernandez, N. [2 ]
van der Schalie, R. [3 ,4 ]
Al Bitar, A. [2 ]
Mialon, A. [2 ]
Richaume, P. [2 ]
Dolman, A. [3 ]
Ducharne, A. [5 ]
机构
[1] INRA, ISPA, UMR1391, Villenave Dornon, France
[2] UPS, CNRS, CESBIO, CNES,IRD,UMR 5126, Toulouse, France
[3] VU Univ Amsterdam VUA, Fac Earth & Life Sci, Amsterdam, Netherlands
[4] Transmissivity BV, Space Technol Ctr, Noordwijk, Netherlands
[5] UPMC, Univ Paris 04, UMR METIS 7619, CNRS,EPHE, Paris, France
关键词
SMOS; AMSR-E; Soil moisture; Statistical regression; CATCHMENT-BASED APPROACH; LAND-SURFACE PROCESSES; AMSR-E; IN-SITU; TEMPORAL RESOLUTION; RETRIEVAL ALGORITHM; SMOS; MODEL; EMISSION; PRODUCTS;
D O I
10.1016/j.rse.2015.11.022
中图分类号
X [环境科学、安全科学];
学科分类号
08 ; 0830 ;
摘要
Within the framework of the efforts of the European Space Agency (ESA) to develop the most consistent and complete record of surface soil moisture (SSM), this study investigated a statistical approach to retrieve a global and long-term SSM dataset from space-borne observations. More specifically, this study investigated the ability of physically based statistical regressions to retrieve SSM from two passive microwave remote sensing observations: the Advanced Microwave Scanning Radiometer (AMSR-E; 2003-Sept. 2011) and the Soil Moisture and Ocean Salinity (SMOS) satellite. Regression coefficients were calibrated using AMSR-E horizontal and vertical brightness temperature (TB) observations and SMOS level 3 SSM (SMOSL3; as a training dataset). This calibration process was carried out over the June 2010-Sept. 2011 period, over which both SMOS and AMSR-E observations coincide. Based on these calibrated coefficients, a global SSM product (referred here to as AMSR-reg) was computed from the AMSR-E TB observations during the 2003-2011 period. The regression quality was assessed by evaluating the AMSR-reg SSM product against the SMOSL3 SSM product over the period of calibration, in terms of correlation (R) and Root Mean Square Error (RMSE). A good agreement (mean global R = 0.60 and mean global RMSE = 0.057 m(3)/m(3)), was obtained between the AMSR-reg and SMOSL3 SSM products particularly over Australia, central USA, central Asia, and the Sahel. In a second step, the AMSR-reg SSM retrievals and commonly used AMSR-E SSM retrievals derived from the Land Parameter Retrieval Model (AMSR-LPRM), were evaluated against two kinds of SSM references (i) the global MERRA-Land SSM simulations and (ii) in situ measurements over 2003-2009. The results demonstrated that both AMSR-reg and AMSR-LPRM (better when considering global simulations) successfully captured the temporal dynamics of the references used having comparable correlation values. AMSR-reg was more consistent with MERRA-land than AMSR-LPRM in terms of unbiased RMSE (ubRMSE) with a global average of ubRMSE of 0.055 m(3)/m(3) for AMSR-reg and 0.084 m(3)/m(3) for AMSRLPRM. In conclusion, the statistical regression, which is tested here for the first time using long-term spaceborne TB datasets, appears to be a promising approach for retrieving SSM from passive microwave remote sensing TB observations. (C)2015 Elsevier Inc. All rights reserved.
引用
收藏
页码:453 / 464
页数:12
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