Abstract

Progress in sensor technologies has allowed real-time monitoring of soil water. It is a challenge to model soil water content based on remote sensing data. Here, we retrieved and modeled surface soil moisture (SSM) at the U.S. Climate Reference Network (USCRN) stations using Sentinel-1 backscatter data from 2016 to 2018 and ancillary data. Empirical machine learning models were established between soil water content measured at the USCRN stations with Sentinel-1 data from 2016 to 2017, the National Land Cover Dataset, terrain parameters, and Polaris soil data, and were evaluated in 2018 at the same USCRN stations. The Cubist model performed better than the multiple linear regression (MLR) and Random Forest (RF) model (R2 = 0.68 and RMSE = 0.06 m3 m-3 for validation). The Cubist model performed best in Shrub/Scrub, followed by Herbaceous and Cultivated Crops but poorly in Hay/Pasture. The success of SSM retrieval was mostly attributed to soil properties, followed by Sentinel-1 backscatter data, terrain parameters, and land cover. The approach shows the potential for retrieving SSM using Sentinel-1 data in a combination of high-resolution ancillary data across the conterminous United States (CONUS). Future work is required to improve the model performance by including more SSM network measurements, assimilating Sentinel-1 data with other microwave, optical and thermal remote sensing products. There is also a need to improve the spatial resolution and accuracy of land surface parameter products (e.g., soil properties and terrain parameters) at the regional and global scales.

Highlights

  • Soil moisture serves an important role in regulating water and energy transport [1,2,3,4]

  • To resample the 10-m backscatter images to the 30-m scale. We describe this briefly here: First, dynamic masks were applied to the raw images to exclude the backscatter values larger than –5 dB and smaller than –20 dB for the VV mode and to exclude the backscatter values larger than –10 dB and smaller than –30 dB for the VH mode

  • Empirical models are established for predicting surface soil moisture (SSM, 0–0.05 m) in 2018 based on historical (2016–2017) Sentinel-1 and ancillary data at the U.S Climate Reference Network soil moisture

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Summary

Introduction

Soil moisture serves an important role in regulating water and energy transport [1,2,3,4] It is considered as a key variable in agriculture, hydrology, atmospheric and climate sciences [5,6]. Real-time soil moisture monitoring enables validation of satellite soil moisture monitoring missions across the globe [10] and creating gridded soil moisture maps at the regional-scale [11]. Both these studies often have a coarse spatial resolution, which does not apply to the field scale. Characterizing soil moisture dynamics and distribution at large spatial and temporal scales is not easy, as it is affected by various physical processes (e.g., precipitation, evapotranspiration, runoff, drainage) and environmental controlling factors (e.g., meteorological forcing, soil texture, vegetation, topography) [7]

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