Validation of Soil Moisture and Ocean Salinity (SMOS) Soil Moisture Over Watershed Networks in the U.S.

被引:290
作者
Jackson, Thomas J. [1 ]
Bindlish, Rajat [1 ]
Cosh, Michael H. [1 ]
Zhao, Tianjie [1 ]
Starks, Patrick J. [2 ]
Bosch, David D. [3 ]
Seyfried, Mark [4 ]
Moran, Mary Susan [5 ]
Goodrich, David C. [5 ]
Kerr, Yann H. [6 ]
Leroux, Delphine [6 ]
机构
[1] ARS, Hydrol & Remote Sensing Lab, USDA, Beltsville, MD 20705 USA
[2] ARS, Grazinglands Res Lab, USDA, El Reno, OK 73036 USA
[3] ARS, SE Watershed Res Ctr, USDA, Tifton, GA 31793 USA
[4] ARS, NW Watershed Res Ctr, USDA, Boise, ID 83712 USA
[5] ARS, SW Watershed Res Ctr, USDA, Tucson, AZ 85719 USA
[6] Ctr Etud Spatiales BIOsphere CESBIO, F-31401 Toulouse, France
来源
IEEE TRANSACTIONS ON GEOSCIENCE AND REMOTE SENSING | 2012年 / 50卷 / 05期
关键词
Advanced Microwave Scanning Radiometer (AMSR-E); passive microwave; Soil Moisture and Ocean Salinity (SMOS); soil moisture; validation; RADIOMETRY; RETRIEVAL; STABILITY; ALGORITHM;
D O I
10.1109/TGRS.2011.2168533
中图分类号
P3 [地球物理学]; P59 [地球化学];
学科分类号
0708 ; 070902 ;
摘要
Estimation of soil moisture at large scale has been performed using several satellite-based passive microwave sensors and a variety of retrieval methods over the past two decades. The most recent source of soil moisture is the European Space Agency Soil Moisture and Ocean Salinity (SMOS) mission. A thorough validation must be conducted to insure product quality that will, in turn, support the widespread utilization of the data. This is especially important since SMOS utilizes a new sensor technology and is the first passive L-band system in routine operation. In this paper, we contribute to the validation of SMOS using a set of four in situ soil moisture networks located in the U. S. These ground-based observations are combined with retrievals based on another satellite sensor, the Advanced Microwave Scanning Radiometer (AMSR-E). The watershed sites are highly reliable and address scaling with replicate sampling. Results of the validation analysis indicate that the SMOS soil moisture estimates are approaching the level of performance anticipated, based on comparisons with the in situ data and AMSR-E retrievals. The overall root-mean-square error of the SMOS soil moisture estimates is 0.043 m(3)/m(3) for the watershed networks (ascending). There are bias issues at some sites that need to be addressed, as well as some outlier responses. Additional statistical metrics were also considered. Analyses indicated that active or recent rainfall can contribute to interpretation problems when assessing algorithm performance, which is related to the contributing depth of the satellite sensor. Using a precipitation flag can improve the performance. An investigation of the vegetation optical depth (tau) retrievals provided by the SMOS algorithm indicated that, for the watershed sites, these are not a reliable source of information about the vegetation canopy. The SMOS algorithms will continue to be refined as feedback from validation is evaluated, and it is expected that the SMOS estimates will improve.
引用
收藏
页码:1530 / 1543
页数:14
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