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An Illustration of FY-3E GNOS-R for Global Soil Moisture Monitoring

An effective soil moisture retrieval method for FY-3E (Fengyun-3E) GNOS-R (GNSS occultation sounder II-reflectometry) is developed in this paper. Here, the LAGRS model, which is totally oriented for GNOS-R, is employed to estimate vegetation and surface roughness effects on surface reflectivity. Sin...

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Autores principales: Yang, Guanglin, Du, Xiaoyong, Huang, Lingyong, Wu, Xuerui, Sun, Ling, Qi, Chengli, Zhang, Xiaoxin, Wang, Jinsong, Song, Shaohui
Formato: Online Artículo Texto
Lenguaje:English
Publicado: MDPI 2023
Materias:
Acceso en línea:https://www.ncbi.nlm.nih.gov/pmc/articles/PMC10347166/
https://www.ncbi.nlm.nih.gov/pubmed/37447675
http://dx.doi.org/10.3390/s23135825
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author Yang, Guanglin
Du, Xiaoyong
Huang, Lingyong
Wu, Xuerui
Sun, Ling
Qi, Chengli
Zhang, Xiaoxin
Wang, Jinsong
Song, Shaohui
author_facet Yang, Guanglin
Du, Xiaoyong
Huang, Lingyong
Wu, Xuerui
Sun, Ling
Qi, Chengli
Zhang, Xiaoxin
Wang, Jinsong
Song, Shaohui
author_sort Yang, Guanglin
collection PubMed
description An effective soil moisture retrieval method for FY-3E (Fengyun-3E) GNOS-R (GNSS occultation sounder II-reflectometry) is developed in this paper. Here, the LAGRS model, which is totally oriented for GNOS-R, is employed to estimate vegetation and surface roughness effects on surface reflectivity. Since the LAGRS (land surface GNSS reflection simulator) model is a space-borne GNSS-R (GNSS reflectometry) simulator based on the microwave radiative transfer equation model, the method presented in this paper takes more consideration on the physical scattering properties for retrieval. Ancillary information from SMAP (soil moisture active passive) such as the vegetation water content and the roughness coefficient are investigated for the final algorithm’s development. At first, the SR (surface reflectivity) data calculated from GNOS-R is calculated and then calibrated, and then the vegetation roughness factor is achieved and used to eliminate the effects on both factors. After receiving the Fresnel reflectivity, the corresponding soil moisture estimated from this method is retrieved. The results demonstrate good consistency between soil moisture derived from GNOS-R data and SMAP soil moisture, with a correlation coefficient of 0.9599 and a root mean square error of 0.0483 cm(3)/cm(3). This method succeeds in providing soil moisture on a global scale and is based on the previously developed physical LAGRS model. In this way, the great potential of GNOS-R for soil moisture estimation is presented.
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spelling pubmed-103471662023-07-15 An Illustration of FY-3E GNOS-R for Global Soil Moisture Monitoring Yang, Guanglin Du, Xiaoyong Huang, Lingyong Wu, Xuerui Sun, Ling Qi, Chengli Zhang, Xiaoxin Wang, Jinsong Song, Shaohui Sensors (Basel) Article An effective soil moisture retrieval method for FY-3E (Fengyun-3E) GNOS-R (GNSS occultation sounder II-reflectometry) is developed in this paper. Here, the LAGRS model, which is totally oriented for GNOS-R, is employed to estimate vegetation and surface roughness effects on surface reflectivity. Since the LAGRS (land surface GNSS reflection simulator) model is a space-borne GNSS-R (GNSS reflectometry) simulator based on the microwave radiative transfer equation model, the method presented in this paper takes more consideration on the physical scattering properties for retrieval. Ancillary information from SMAP (soil moisture active passive) such as the vegetation water content and the roughness coefficient are investigated for the final algorithm’s development. At first, the SR (surface reflectivity) data calculated from GNOS-R is calculated and then calibrated, and then the vegetation roughness factor is achieved and used to eliminate the effects on both factors. After receiving the Fresnel reflectivity, the corresponding soil moisture estimated from this method is retrieved. The results demonstrate good consistency between soil moisture derived from GNOS-R data and SMAP soil moisture, with a correlation coefficient of 0.9599 and a root mean square error of 0.0483 cm(3)/cm(3). This method succeeds in providing soil moisture on a global scale and is based on the previously developed physical LAGRS model. In this way, the great potential of GNOS-R for soil moisture estimation is presented. MDPI 2023-06-22 /pmc/articles/PMC10347166/ /pubmed/37447675 http://dx.doi.org/10.3390/s23135825 Text en © 2023 by the authors. https://creativecommons.org/licenses/by/4.0/Licensee MDPI, Basel, Switzerland. This article is an open access article distributed under the terms and conditions of the Creative Commons Attribution (CC BY) license (https://creativecommons.org/licenses/by/4.0/).
spellingShingle Article
Yang, Guanglin
Du, Xiaoyong
Huang, Lingyong
Wu, Xuerui
Sun, Ling
Qi, Chengli
Zhang, Xiaoxin
Wang, Jinsong
Song, Shaohui
An Illustration of FY-3E GNOS-R for Global Soil Moisture Monitoring
title An Illustration of FY-3E GNOS-R for Global Soil Moisture Monitoring
title_full An Illustration of FY-3E GNOS-R for Global Soil Moisture Monitoring
title_fullStr An Illustration of FY-3E GNOS-R for Global Soil Moisture Monitoring
title_full_unstemmed An Illustration of FY-3E GNOS-R for Global Soil Moisture Monitoring
title_short An Illustration of FY-3E GNOS-R for Global Soil Moisture Monitoring
title_sort illustration of fy-3e gnos-r for global soil moisture monitoring
topic Article
url https://www.ncbi.nlm.nih.gov/pmc/articles/PMC10347166/
https://www.ncbi.nlm.nih.gov/pubmed/37447675
http://dx.doi.org/10.3390/s23135825
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