TY - JOUR
T1 - Uncertainty of reference pixel soil moisture averages sampled at SMAP core validation sites
AU - Chen, Fan
AU - Crow, Wade T.
AU - Cosh, Michael H.
AU - Colliander, Andreas
AU - Asanuma, Jun
AU - Berg, Aaron
AU - Bosch, David D.
AU - Caldwell, Todd G.
AU - Collins, Chandra Holifield
AU - Jensen, Karsten Høgh
AU - Martínez-Fernández, Jose
AU - McNairn, Heather
AU - Starks, Patrick J.
AU - Su, Zhongbo
AU - Walker, Jeffrey P.
N1 - Funding Information:
This study is supported by Dr. Wade Crow?s membership on the NASA Soil Moisture Active Passive mission. A partial contribution to this work was made at Jet Propulsion Laboratory, California Institute of Technology, under a contract with the National Aeronautics and Space Administration. USDA is an equal opportunity provider and employer. The REMEDHUS network data was provided by the University of Salamanca team supported by the Spanish Ministry of Economy and Competitiveness with the project ESP2017-89463-C3-3-R, and the European Regional Development Fund (ERDF). The Twente network was supported by the Netherlands Organization for Scientific Research (Project No. ALW-GO/14-29) and the ESA MOST Dragon IV program [Monitoring Water and Energy Cycles at Climate Scale in the Third Pole Environment (CLIMATE-TPE)]. The authors are grateful to ESA for offering the ELBARA-III radiometer (ZS). Erica Tetlock from Environment and Climate Change Canada and Tracy Rowlandson are acknowledged for work with the Kenaston Network with funding from Environment and Climate Change Canada, the Canadian Space Agency, and the Natural Sciences and Engineering Research Council of Canada. The VILLUM Foundation provided funding for the HOBE observatory.
Publisher Copyright:
© 2019 American Meteorological Society.
PY - 2019/8
Y1 - 2019/8
N2 - Despite extensive efforts to maximize ground coverage and improve upscaling functions within core validation sites (CVS) of the NASA Soil Moisture Active Passive (SMAP) mission, spatial averages of point-scale soil moisture observations often fail to accurately capture the true average of the reference pixels. Therefore, some level of pixel-scale sampling error from in situ observations must be considered during the validation of SMAP soil moisture retrievals. Here, uncertainties in the SMAP core site average soil moisture (CSASM) due to spatial sampling errors are examined and their impact on CSASM-based SMAP calibration and validation metrics is discussed. The estimated uncertainty (due to spatial sampling limitations) of mean CSASM over time is found to be large, translating into relatively large sampling uncertainty levels for SMAP retrieval bias when calculated against CSASM. As a result, CSASM-based SMAP bias estimates are statistically insignificant at nearly all SMAP CVS. In addition, observations from temporary networks suggest that these (already large) bias uncertainties may be underestimated due to undersampled spatial variability. The unbiased root-mean-square error (ubRMSE) of CSASM is estimated via two approaches: classical sampling theory and triple collocation, both of which suggest that CSASM ubRMSE is generally within the range of 0.01–0.02 m3 m-3. Although limitations in both methods likely lead to underestimation of ubRMSE, the results suggest that CSASM captures the temporal dynamics of the footprint-scale soil moisture relatively well and is thus a reliable reference for SMAP ubRMSE calculations. Therefore, spatial sampling errors are revealed to have very different impacts on efforts to estimate SMAP bias and ubRMSE metrics using CVS data.
AB - Despite extensive efforts to maximize ground coverage and improve upscaling functions within core validation sites (CVS) of the NASA Soil Moisture Active Passive (SMAP) mission, spatial averages of point-scale soil moisture observations often fail to accurately capture the true average of the reference pixels. Therefore, some level of pixel-scale sampling error from in situ observations must be considered during the validation of SMAP soil moisture retrievals. Here, uncertainties in the SMAP core site average soil moisture (CSASM) due to spatial sampling errors are examined and their impact on CSASM-based SMAP calibration and validation metrics is discussed. The estimated uncertainty (due to spatial sampling limitations) of mean CSASM over time is found to be large, translating into relatively large sampling uncertainty levels for SMAP retrieval bias when calculated against CSASM. As a result, CSASM-based SMAP bias estimates are statistically insignificant at nearly all SMAP CVS. In addition, observations from temporary networks suggest that these (already large) bias uncertainties may be underestimated due to undersampled spatial variability. The unbiased root-mean-square error (ubRMSE) of CSASM is estimated via two approaches: classical sampling theory and triple collocation, both of which suggest that CSASM ubRMSE is generally within the range of 0.01–0.02 m3 m-3. Although limitations in both methods likely lead to underestimation of ubRMSE, the results suggest that CSASM captures the temporal dynamics of the footprint-scale soil moisture relatively well and is thus a reliable reference for SMAP ubRMSE calculations. Therefore, spatial sampling errors are revealed to have very different impacts on efforts to estimate SMAP bias and ubRMSE metrics using CVS data.
KW - 22/4 OA procedure
UR - http://www.scopus.com/inward/record.url?scp=85073326001&partnerID=8YFLogxK
U2 - 10.1175/JHM-D-19-0049.1
DO - 10.1175/JHM-D-19-0049.1
M3 - Article
AN - SCOPUS:85073326001
VL - 20
SP - 1553
EP - 1569
JO - Journal of hydrometeorology
JF - Journal of hydrometeorology
SN - 1525-755X
IS - 8
ER -