Abstract

The combined influence of surface soil moisture and roughness on radar backscatters has been limiting SAR’s application in soil moisture retrieval. In the past research, multi-temporal analysis and artificial neural network (ANN) inversion of physically based forward models were regarded as promising methods to decouple that combined influence. However, the former does not consider soil roughness change over a relatively longer period and the latter makes it hard to thoroughly eliminate the effect of soil roughness. This study proposes to use generalized regression neural network (GRNN) to derive bare surface soil moisture (BSSM) from radar backscatter observations regardless of the effect of soil roughness (GRNN inversion of backscatter observations). This method not only can derive BSSM from radar backscatters, provided soil roughness is unknown in any long period, but also can train models based on small-size sample data so as to reduce the manual error of training data created by simulation of physically based models. The comparison of validations between BSSM-backscatter models and BSSM-roughness-backscatter models both analyzed by GRNN shows that the incorporation of soil roughness cannot raise the prediction accuracy of models and, instead, even reduce it, indicating that the combined influence is thoroughly decoupled when being analyzed by GRNN. Moreover, BSSM-backscatter models by GRNN are recommended due to their good prediction, even compared to those related models in past publications.

Highlights

  • That methodology is under the assumption that soil roughness is constant within a sufficiently short time interval or soil roughness changes over a longer time scale compared to bare surface soil moisture (BSSM) change, and synthetic aperture radar (SAR) backscatter change is just related to BSSM change during this period, under the given radar configurations and homogeneous soil textures

  • Artificial neural network (ANN) inversion of physically based forward electromagnetic models has been realized ably to retrieve BSSM, provided that surface roughness is an unknown parameter in the training (e.g., Weimann, 1998; Baghdadi et al, 2002; Paloscia et al, 2008, 2013; Santi et al, 2016)

  • Fifteen BSSM-backscatter models are constructed by generalized regression neural network (GRNN) here, based on 15 combinations of full-polarized backscattering coefficients: {σohh }, {σovv }, {σohv}, {σovh}, {σohh, σovv}, {σohh, σohv}, {σohh, σovh}, {σovv, σovh}, {σovv, σohv}, {σohv, σovh}, {σohh, σovv, σohv}, {σohh, σovv, σovh}, {σohh, σohv, σovh}, {σovv, σohv, σovh}, and {σohh, σovv, σohv, σovh}

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Summary

Introduction

The verified combination of influence of bare surface soil moisture (BSSM) and roughness on backscattering coefficients of synthetic aperture radar (SAR) especially at the C-band, under given radar parameters and homogeneous soil textures, has been limiting its application as an operational source of soil moisture in hydrology, though it is regarded as the most suitable for monitoringBare Surface Soil Moisture Retrieval surface soil moisture (SSM), due to its high sensitivity to water contents, its high spatial resolution in the order of tens of meters for the distributed soil moisture, and its ability to neglect the influence of the atmosphere (Ulaby et al, 1982; Fung and Chen, 1994; Nancy and James, 2003; Wagner et al, 2007; Kornelsen and Coulibaly, 2013; Peng et al, 2017; Zeng et al, 2020). Artificial neural network (ANN) inversion of physically based forward electromagnetic models has been realized ably to retrieve BSSM, provided that surface roughness is an unknown parameter in the training (e.g., Weimann, 1998; Baghdadi et al, 2002; Paloscia et al, 2008, 2013; Santi et al, 2016) These physically based models account for the interactions between the microwave radiation and soil [e.g., the integral equation model (IEM) by Fung et al (1992) and the advanced integral equation model (AIEM) by Wu et al (2001)] and ably simulate backscattering coefficients in terms of soil attributes (e.g., the dielectric constant and the surface roughness). This contrast indicates that in spite of the good prediction accuracy for SSM retrieval by ANN inversion of physical-based forward models, this method does not thoroughly decouple the effect of BSSM on backscatter from that of soil roughness but just reduces the effect of soil roughness on BSSM retrieval from backscatter

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