Modeling Surface Roughness to Estimate Surface Moisture Using Radarsat-2 Quad Polarimetric SAR Data

6th Asian Physics Symposium

Nurtyawan, R.^1 ; Saepuloh, A.^1 ; Budiharto, A.^1 ; Wikantika, K.^1

Centre for Remote Sensing (CRS), Institute of Technology Bandung, Jl. Ganesha No. 10, Bandung, Indonesia^1

关键词: Backscattering coefficients;    Backscattering intensity;    Coefficient of determination;    Microwave backscattering;    Polarimetric synthetic aperture radars;    Radar backscattering coefficient;    Surface roughness model;    Third degree polynomial;   

Others  :  https://iopscience.iop.org/article/10.1088/1742-6596/739/1/012105/pdf
DOI  :  10.1088/1742-6596/739/1/012105

来源: IOP

【 摘 要 】

Microwave backscattering from the earth's surface depends on several parameters such as surface roughness and dielectric constant of surface materials. The two parameters related to water content and porosity are crucial for estimating soil moisture. The soil moisture is an important parameter for ecological study and also a factor to maintain energy balance of land surface and atmosphere. Direct roughness measurements to a large area require extra time and cost. Heterogeneity roughness scale for some applications such as hydrology, climate, and ecology is a problem which could lead to inaccuracies of modeling. In this study, we modeled surface roughness using Radasat-2 quad Polarimetric Synthetic Aperture Radar (PolSAR) data. The statistical approaches to field roughness measurements were used to generate an appropriate roughness model. This modeling uses a physical SAR approach to predicts radar backscattering coefficient in the parameter of radar configuration (wavelength, polarization, and incidence angle) and soil parameters (surface roughness and dielectric constant). Surface roughness value is calculated using a modified Campbell and Shepard model in 1996. The modification was applied by incorporating the backscattering coefficient (σ°) of quad polarization HH, HV and VV. To obtain empirical surface roughness model from SAR backscattering intensity, we used forty-five sample points from field roughness measurements. We selected paddy field in Indramayu district, West Java, Indonesia as the study area. This area was selected due to intensive decreasing of rice productivity in the Northern Coast region of West Java. Third degree polynomial is the most suitable data fitting with coefficient of determination R2and RMSE are about 0.82 and 1.18 cm, respectively. Therefore, this model is used as basis to generate the map of surface roughness.