Enhancing Soil Moisture Active–Passive Estimates with Soil Moisture Active–Passive Reflectometer Data Using Graph Signal Processing

Author:

Garcia-Cardona Johanna1,Rodriguez-Alvarez Nereida2ORCID,Munoz-Martin Joan Francesc3ORCID,Bosch-Lluis Xavier3ORCID,Oudrhiri Kamal4

Affiliation:

1. Department of Electrical and Computer Engineering, University of Southern California, Los Angeles, CA 90089, USA

2. Planetary Radar and Radio Sciences Group, Jet Propulsion Laboratory, California Institute of Technology, Pasadena, CA 91109, USA

3. Signal Processing and Networks Group, Jet Propulsion Laboratory, California Institute of Technology, Pasadena, CA 91109, USA

4. Communication Architectures and Research Section, Jet Propulsion Laboratory, California Institute of Technology, Pasadena, CA 91109, USA

Abstract

The Soil Moisture Active–Passive (SMAP) mission has greatly contributed to the use of remote sensing technologies for monitoring the Earth’s land surface and estimating geophysical parameters that influence the climate system. Since the SMAP mission switched its radar receiver to allow the reception of Global Positioning System (GPS) signals, Global Navigation Satellite System Reflectometry (GNSS-R) configuration has been enabled, providing full polarimetric forward scattering measurements of the Earth’s surface, also known as SMAP Reflectometry or SMAP-R. Polarimetric GNSS-R is beneficial for sensing land surface properties, especially for more accurate estimations of soil moisture (SM) in densely vegetated areas. In this study, we explore the opportunity to enhance SMAP mission soil moisture estimates using reflected GNSS signals. We achieve this by interpolating the sparse reflectivity data with terrain information to disaggregate radiometer brightness temperatures. Our main objective is to present a novel algorithm based on Graph Signal Processing (GSP) that uses reflectometry data to enhance SMAP radiometer observations and ultimately improve SM retrievals. By implementing methods from the GSP field, we formulate the reflectivity interpolation problem as a signal reconstruction on a graph, where the weights of the edges between the nodes are chosen as a function of geophysical information. Subsequently, using the retrieved reflectivity maps, we increase the resolution of the brightness temperature data, leading to an improvement in the SM estimates. Initial findings indicate that our GSP method presents a promising alternative for analyzing sparse remote sensing observations, leveraging Earth’s surface geophysical information. This approach results in a notable improvement, with a reduced Root Mean Square Error (RMSE) of 11.8% compared to SMAP data and a reduction in unbiased RMSE (uRMSE) by 14.7% over vegetated areas.

Funder

National Aeronautics and Space Administration through the Research Opportunities in Space and Earth Sciences

ROSES NRA Program

Publisher

MDPI AG

Reference28 articles.

1. (2023, September 26). The Global Climate Observing System (GCOS) What are Essential Climate Variables?. Available online: https://gcos.wmo.int/en/essential-climate-variables/about.

2. Eroglu, O., Kurum, M., Boyd, D., and Gurbuz, A.C. (2019). High spatio-temporal resolution cygnss soil moisture estimates using artificial neural networks. Remote Sens., 11.

3. A review of the methods available for estimating soil moisture and its implications for water resource management;Dobriyal;J. Hydrol.,2012

4. The SMOS Soil Moisture Retrieval Algorithm;Kerr;IEEE Trans. Geosci. Remote Sens.,2012

5. The Soil Moisture Active Passive (SMAP) Mission;Entekhabi;Proc. IEEE,2010

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