Abstract

The objective of this paper is to extend the semi-empirical calibration of the backscattering Integral Equation Model (IEM) initially proposed for Synthetic Aperture Radar (SAR) data at C- and X-bands to SAR data at L-band. A large dataset of radar signal and in situ measurements (soil moisture and surface roughness) over bare soil surfaces were used. This dataset was collected over numerous agricultural study sites in France, Luxembourg, Belgium, Germany and Italy using various SAR sensors (AIRSAR, SIR-C, JERS-1, PALSAR-1, ESAR). Results showed slightly better simulations with exponential autocorrelation function than with Gaussian function and with HH than with VV. Using the exponential autocorrelation function, the mean difference between experimental data and Integral Equation Model (IEM) simulations is +0.4 dB in HH and −1.2 dB in VV with a Root Mean Square Error (RMSE) about 3.5 dB. In order to improve the modeling results of the IEM for a better use in the inversion of SAR data, a semi-empirical calibration of the IEM was performed at L-band in replacing the correlation length derived from field experiments by a fitting parameter. Better agreement was observed between the backscattering coefficient provided by the SAR and that simulated by the calibrated version of the IEM (RMSE about 2.2 dB).

Highlights

  • Soil moisture content and roughness play an important role in hydrology

  • Results showed that Lopt1 values in HH were higher than those in VV for both exponential and Gaussian ACFs, whereas Lopt2 values were similar in HH and VV for both ACFs

  • Increasing of Integral Equation Model (IEM) in the first part of simulations corresponds to very short correlation lengths

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Summary

Introduction

Soil moisture content and roughness play an important role in hydrology. These soil parameters could be estimated using Synthetic Aperture Radar (SAR) irrespective of the meteorological conditions.these estimations require the use of a radar backscattering model that is capable of correctly modeling the radar signal. Soil moisture content and roughness play an important role in hydrology These soil parameters could be estimated using Synthetic Aperture Radar (SAR) irrespective of the meteorological conditions. Most studies reported discrepancies between modeled backscatters by IEM and observed backscatters by SAR sensors at L-, C-, and X-bands [10,11,12,13,14,15,16,17,18,19,20] These discrepancies could be related to the inaccuracy of the roughness measurements, which introduces significant errors into the modeled radar signal [21,22], and to the model itself [10,11,12,13,14,15]. The estimation of soil parameters (moisture content and roughness) from SAR images can be inaccurate using such a model

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