Soil moisture retrieval over agricultural fields from multi-polarized and multi-angular RADARSAT-2 SAR data

被引:176
作者
Gherboudj, Imen [1 ]
Magagi, Ramata [1 ]
Berg, Aaron A. [2 ]
Toth, Brenda [3 ]
机构
[1] Univ Sherbrooke, Ctr Applicat & Rech Teledetect CARTEL, 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
基金
加拿大自然科学与工程研究理事会;
关键词
RADARSAT-2; Polarization ratios; Modelling; Empirical relationships; Ground measurements; Agricultural fields; Crop height; Crop water content; Soil surface roughness; Soil moisture; SYNTHETIC-APERTURE RADAR; INTERFEROMETRIC COHERENCE; VEGETATION CANOPIES; MICROWAVE EMISSION; MODEL; INVERSION; COVER; POLARIZATION; ATTENUATION; PARAMETERS;
D O I
10.1016/j.rse.2010.07.011
中图分类号
X [环境科学、安全科学];
学科分类号
08 ; 0830 ;
摘要
The aim of this study was to estimate soil moisture from RADARSAT-2 Synthetic Aperture Radar (SAR) images acquired over agricultural fields. The adopted approach is based on the combination of semi-empirical backscattering models, four RADARSAT-2 images and coincident ground measurements (soil moisture, soil surface roughness and vegetation characteristics) obtained near Saskatoon, Saskatchewan, Canada during the summer of 2008. The depolarization ratio (chi(v)), the co-polarized correlation coefficient (rho(vvhh)) and the ratio of the absolute value of cross polarization to crop height (Lambda(vh)) derived from RADARSAT-2 data were analyzed with respect to changes in soil surface roughness, crop height, soil moisture and vegetation water content. This sensitivity analysis allowed us to develop empirical relationships for soil surface roughness, crop height and crop water content estimation regardless of crop type. The latter were then used to correct the semi-empirical Water-Cloud model for soil surface roughness and vegetation effects in order to retrieve soil moisture data. The soil moisture retrieved algorithm is evaluated over mature crop fields (wheat, pea, lentil, and canola) using ground measurements. Results show average relative errors of 19%, 10%, 25.5% and 32% respectively for the retrieval of crop height, soil surface roughness, crop water content and soil moisture. (C) 2010 Elsevier Inc. All rights reserved.
引用
收藏
页码:33 / 43
页数:11
相关论文
共 43 条
[21]   A Time-Series Approach to Estimate Soil Moisture Using Polarimetric Radar Data [J].
Kim, Yunjin ;
van Zyl, Jakob J. .
IEEE TRANSACTIONS ON GEOSCIENCE AND REMOTE SENSING, 2009, 47 (08) :2519-2527
[22]  
KIRDYASHEV KP, 1979, RADIOTEKH ELEKTRON+, V24, P256
[23]   INTENSITY AND PHASE STATISTICS OF MULTILOOK POLARIMETRIC AND INTERFEROMETRIC SAR IMAGERY [J].
LEE, JS ;
HOPPEL, KW ;
MANGO, SA ;
MILLER, AR .
IEEE TRANSACTIONS ON GEOSCIENCE AND REMOTE SENSING, 1994, 32 (05) :1017-1028
[24]   Monitoring Sugarcane Growth Using ENVISAT ASAR Data [J].
Lin, Hui ;
Chen, Jinsong ;
Pei, Zhiyuan ;
Zhang, Songling ;
Hu, Xianzhi .
IEEE TRANSACTIONS ON GEOSCIENCE AND REMOTE SENSING, 2009, 47 (08) :2572-2580
[25]  
McNairn H., 2009, P IGARSS 09 JUL 12 1, VII, P898
[26]   Quantitative retrieval of soil moisture content and surface roughness from multipolarized radar observations of bare soil surfaces [J].
Oh, Y .
IEEE TRANSACTIONS ON GEOSCIENCE AND REMOTE SENSING, 2004, 42 (03) :596-601
[27]   AN EMPIRICAL-MODEL AND AN INVERSION TECHNIQUE FOR RADAR SCATTERING FROM BARE SOIL SURFACES [J].
OH, Y ;
SARABANDI, K ;
ULABY, FT .
IEEE TRANSACTIONS ON GEOSCIENCE AND REMOTE SENSING, 1992, 30 (02) :370-381
[28]   A methodology for surface soil moisture and vegetation optical depth retrieval using the microwave polarization difference index [J].
Owe, M ;
de Jeu, R ;
Walker, J .
IEEE TRANSACTIONS ON GEOSCIENCE AND REMOTE SENSING, 2001, 39 (08) :1643-1654
[29]   ESTIMATING THE CHARACTERISTICS OF VEGETATION CANOPIES WITH AIRBORNE RADAR MEASUREMENTS [J].
PREVOT, L ;
DECHAMBRE, M ;
TACONET, O ;
VIDALMADJAR, D ;
NORMAND, M ;
GALLE, S .
INTERNATIONAL JOURNAL OF REMOTE SENSING, 1993, 14 (15) :2803-2818
[30]  
Romshoo S. A., 2002, J INDIAN SOC REMOTE, V30, P229, DOI DOI 10.1007/BF03000366