Validation of SMOS Data Over Agricultural and Boreal Forest Areas in Canada

被引:62
作者
Gherboudj, Imen [1 ]
Magagi, Ramata [1 ]
Goita, Kalifa [1 ]
Berg, Aaron A. [2 ]
Toth, Brenda [3 ]
Walker, Anne [3 ]
机构
[1] Univ Sherbrooke, Dept Geomat Appl, Sherbrooke, PQ J1K 2R1, Canada
[2] Univ Guelph, Dept Geog, Guelph, ON N1G 2W1, Canada
[3] Environm Canada, MSC Hydrometeorol & Arctic Lab, Saskatoon, SK S7N 3H5, Canada
来源
IEEE TRANSACTIONS ON GEOSCIENCE AND REMOTE SENSING | 2012年 / 50卷 / 05期
基金
美国国家航空航天局; 加拿大自然科学与工程研究理事会;
关键词
Agricultural and forested areas; brightness temperature; ground and airborne measurements; modeling; soil moisture; Soil Moisture and Ocean Salinity (SMOS); validation; SOIL-MOISTURE RETRIEVALS; BAND MICROWAVE EMISSION; AMSR-E; SURFACE-ROUGHNESS; BRIGHTNESS TEMPERATURES; AIRBORNE DATA; MODEL; PARAMETERIZATION; VEGETATION; ALGORITHM;
D O I
10.1109/TGRS.2012.2188532
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
This study was conducted as part of the Soil Moisture and Ocean Salinity (SMOS) calibration and validation activities over agricultural and boreal forest sites located in Saskatchewan, Canada. For each site covering 33 km x 71 km (i.e., about two SMOS pixels), we examined the SMOS brightness temperature (L1c) and soil moisture (L2) products from May 1 to September 30, 2010. The consistency of these data with respect to theory and to the temporal variation of surface characteristics was first discussed at both sites. Then, the SMOS L1c (prototype 346) and L2 (prototypes 305-309) products were evaluated using the Canadian Experiment for Soil Moisture in 2010 (CanEx-SM10) ground measurements and L-band passive microwave airborne measurements, in addition to AMSR-E soil moisture estimates and simulations from the zeroth order tau - omega radiative transfer model. For both study sites, the model underestimated SMOS brightness temperatures in V polarization, whereas an overestimation was observed in H polarization. The data sets showed that both the SMOS and AMSR-E soil moisture values were underestimated compared with ground measurements collected during CanEx-SM10 but less so for the AMSR-E estimates. The SMOS soil moisture product was underestimated with a RMSE varying from 0.15 to 0.18 m(3)/m(3). Furthermore, the overall results showed that errors in the soil moisture estimates increased with the absolute value of soil moisture.
引用
收藏
页码:1623 / 1635
页数:13
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