Zheng et al. (2025) Modeling, prediction, and retrieval of surface soil moisture from InSAR closure phase
Identification
- Journal: Remote Sensing of Environment
- Year: 2025
- Date: 2025-11-04
- Authors: Yujie Zheng, Heresh Fattahi
- DOI: 10.1016/j.rse.2025.115104
Research Groups
- Department of Sustainable Earth System Sciences, University of Texas at Dallas, USA
- Jet Propulsion Laboratory, California Institute of Technology, USA
Short Summary
This study presents a discretized, multi-layer soil moisture model that links soil moisture variability to single-look SAR measurements and their closure phase. It introduces a scalable algorithm for retrieving a relative InSAR Soil Moisture Index, demonstrating its potential for large-scale soil moisture monitoring through validation against in situ and satellite data.
Objective
- To develop a discretized, multi-layer soil moisture model that links soil moisture variability to single-look Synthetic Aperture Radar (SAR) measurements and their closure phase.
- To identify distinct closure phase signatures arising from variations in soil moisture, radar frequencies, and soil textures.
- To introduce and validate a scalable algorithm for retrieving the InSAR Soil Moisture Index, a relative soil moisture product, using InSAR closure phase.
Study Configuration
- Spatial Scale: Regional (Mojave Desert and Central Valley in California) with potential for large-scale monitoring at high resolution (tens of meters).
- Temporal Scale: Not explicitly defined for a specific study period, but the methodology involves analyzing variations in soil moisture over time using multiple SAR acquisitions for closure phase calculation.
Methodology and Data
- Models used: Discretized, multi-layer soil moisture model; approximate transfer function between soil moisture anomalies and closure phase responses.
- Data sources: Single-look SAR measurements (including L-band radar), InSAR closure phase, in situ soil moisture measurements, SMAP/Sentinel-1 soil moisture measurements.
Main Results
- The developed model reveals distinct closure phase signatures influenced by soil moisture variability, radar frequencies, and soil textures.
- Positive asymmetric soil moisture anomalies are predicted to produce positive closure phase step-changes, while negative asymmetric anomalies yield negative step-changes, consistent with observed data.
- Low-frequency radar (e.g., L-band) demonstrates heightened sensitivity to the vertical distribution of soil moisture.
- An approximate transfer function between soil moisture anomalies and closure phase responses was identified.
- A scalable algorithm for retrieving the InSAR Soil Moisture Index (a relative soil moisture product) was successfully introduced and demonstrated in two diverse environments (Mojave Desert and Central Valley, California).
- The derived InSAR Soil Moisture Index showed good agreement with both in situ soil moisture measurements and SMAP/Sentinel-1 soil moisture measurements.
Contributions
- Development of a novel discretized, multi-layer soil moisture model that directly links soil moisture variability to single-look SAR measurements and the InSAR closure phase.
- Identification and characterization of distinct closure phase signatures in response to soil moisture changes, radar frequencies, and soil textures.
- Demonstration of the enhanced sensitivity of low-frequency radar (L-band) to the vertical distribution of soil moisture.
- Introduction of a scalable algorithm for retrieving a relative InSAR Soil Moisture Index using closure phase, effectively mitigating the influence of ground deformation and atmospheric delays that challenge traditional InSAR phase methods.
- Validation of the retrieval algorithm in diverse environments, highlighting its potential for accurate, large-scale, and high-resolution soil moisture monitoring.
Funding
Not specified in the provided text.
Citation
@article{Zheng2025Modeling,
author = {Zheng, Yujie and Fattahi, Heresh},
title = {Modeling, prediction, and retrieval of surface soil moisture from InSAR closure phase},
journal = {Remote Sensing of Environment},
year = {2025},
doi = {10.1016/j.rse.2025.115104},
url = {https://doi.org/10.1016/j.rse.2025.115104}
}
Original Source: https://doi.org/10.1016/j.rse.2025.115104