Abstract

Soil moisture is a key part of Earth’s climate systems, including agricultural and hydrological cycles. Soil moisture data from satellite and numerical models is typically provided at a global scale with coarse spatial resolution, which is not enough for local and regional applications. In this study, a soil moisture downscaling model was developed using satellite-derived variables targeting Global Land Data Assimilation System (GLDAS) soil moisture as a reference dataset in East Asia based on the optimization of a modified regression tree. A total of six variables, Advanced Microwave Scanning Radiometer 2 (AMSR2) and Advanced SCATterometer (ASCAT) soil moisture products, Shuttle Radar Topography Mission (SRTM) Digital Elevation Model (DEM), and MODerate resolution Imaging Spectroradiometer (MODIS) products, including Land Surface Temperature, Normalized Difference Vegetation Index, and land cover, were used as input variables. The optimization was conducted through a pruning approach for operational use, and finally 59 rules were extracted based on root mean square errors (RMSEs) and correlation coefficients (r). The developed downscaling model showed a good modeling performance (r = 0.79, RMSE = 0.056 m3·m−3, and slope = 0.74). The 1 km downscaled soil moisture showed similar time series patterns with both GLDAS and ground soil moisture and good correlation with ground soil moisture (average r = 0.47, average RMSD = 0.038 m3·m−3) at 14 ground stations. The spatial distribution of 1 km downscaled soil moisture reflected seasonal and regional characteristics well, although the model did not result in good performance over a few areas such as Southern China due to very high cloud cover rates. The results of this study are expected to be helpful in operational use to monitor soil moisture throughout East Asia since the downscaling model produces daily high resolution (1 km) real time soil moisture with a low computational demand. This study yielded a promising result to operationally produce daily high resolution soil moisture data from multiple satellite sources, although there are yet several limitations. In future research, more variables including Global Precipitation Measurement (GPM) precipitation, Soil Moisture Active Passive (SMAP) soil moisture, and other vegetation indices will be integrated to improve the performance of the proposed soil moisture downscaling model.

Highlights

  • Soil moisture, a key variable of regional and global climate systems, is important to understand the interaction between the land and the atmosphere

  • The optimization was conducted through a pruning approach for operational use, and 59 rules were extracted based on root mean square errors (RMSEs) and correlation coefficients (r)

  • More variables including Global Precipitation Measurement (GPM) precipitation, Soil Moisture Active Passive (SMAP) soil moisture, and other vegetation indices will be integrated to improve the performance of the proposed soil moisture downscaling model

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Summary

Introduction

A key variable of regional and global climate systems, is important to understand the interaction between the land and the atmosphere. Changes in soil moisture have a considerable impact on climate change [1]; hydrological processes, including precipitation, stream flow, and energy fluxes [2,3,4,5,6,7]; agricultural processes such as irrigation management and crop yield prediction [8,9]; and severe weather events such as droughts and heat waves [10,11,12,13,14,15,16]. It is important to monitor temporal and spatial patterns of soil moisture. Soil moisture information has been provided by ground measurements at stations, remote sensing observations, and numerical models. In situ measurements provide accurate soil moisture data for specific locations with high temporal resolution (e.g., 30 min or 1 h). Global in situ soil moisture data can be acquired from the International Soil Moisture Network

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