Abstract

The objective of this paper is to propose a combined approach for the high-precision mapping of soil moisture during the wheat growth cycle based on synthetic aperture radar (SAR) (Radarsat-2) and optical satellite data (Landsat-8). For this purpose, the influence of vegetation was removed from the total backscatter by using the modified water cloud model (MWCM), which takes the vegetation fraction (fveg) into account. The VV/VH polarization radar backscattering coefficients database was established by a numerical simulation based on the advanced integrated equation model (AIEM) and the cross-polarized ratio of the Oh model. Then the empirical relationship between the bare soil backscattering coefficient and both the soil moisture and the surface roughness was developed by regression analysis. The surface roughness in this paper was described by using the effective roughness parameter and the combined roughness form. The experimental results revealed that using effective roughness as the model input instead of in-situ measured roughness can obtain soil moisture with high accuracy and effectively avoid the uncertainty of roughness measurement. The accuracy of soil moisture inversion could be improved by introducing vegetation fraction on the basis of the water cloud model (WCM). There was a good correlation between the estimated soil moisture and the observed values, with a root mean square error (RMSE) of about 4.14% and the coefficient of determination (R2) about 0.7390.

Highlights

  • In agriculture, soil moisture is a basic condition for crop growth and development, and it runs through all aspects of crop growth

  • The vegetation fraction parameter was introduced to the water cloud model (WCM) to distinguish the vegetation scattering contribution from the direct scattering contribution of bare surface, which can more accurately correct the influence of vegetation layer on radar backscatter

  • A new soil moisture inversion method based on modified water cloud model (MWCM) and coupled empirical model (CEM) was obtained, which is abbreviated as MWCM-CEM for the convenience of the following description

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Summary

Introduction

Soil moisture is a basic condition for crop growth and development, and it runs through all aspects of crop growth. Soil moisture is an important index for early warning of crop drought and flood disasters and an important parameter for evaluating crop growth. The estimation and description of the temporal and spatial dynamics of soil moisture are of great significance for hydrology, ecology and agriculture [1,2,3,4,5]. With the development of satellite remote sensing technology, it has become possible to obtain regional soil moisture information. Compared with other remote sensing methods, synthetic aperture radar (SAR) is more suitable for accurate inversion of soil moisture due to its characteristics of all-day, all-weather, high temporal and spatial resolutions. It has been proven that C-band SAR data can detect the soil moisture of 0–5 cm on the surface, because soil moisture seriously affects soil dielectric constant, which is closely related to radar backscatter [6,7,8]

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