A full-polarization GNSS-R Delay-Doppler-Map (DDM) simulator for bare soil freeze/thaw process detection

Abstract The soil freeze/thaw processes have a significant impact on the surface energy and moisture balance, which play a key role in ecosystem diversity and productivity. The air-/space-borne Global Navigation Satellite System (GNSS)-Reflectometry (GNSS-R) is a bistatic radar with receiving power...

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Main Authors: Xuerui Wu, Shuanggen Jin, Xinqiu Ouyang
Format: Article
Language:English
Published: SpringerOpen 2020-03-01
Series:Geoscience Letters
Subjects:
Online Access:http://link.springer.com/article/10.1186/s40562-020-00154-8
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spelling doaj-cf09e17732b8422a9c1b976d5684a2042020-11-25T02:38:06ZengSpringerOpenGeoscience Letters2196-40922020-03-01711910.1186/s40562-020-00154-8A full-polarization GNSS-R Delay-Doppler-Map (DDM) simulator for bare soil freeze/thaw process detectionXuerui Wu0Shuanggen Jin1Xinqiu Ouyang2Shanghai Astronomical Observatory, Chinese Academy of SciencesShanghai Astronomical Observatory, Chinese Academy of SciencesSchool of Geograghy and Planning, Sun Yat-Sen UniversityAbstract The soil freeze/thaw processes have a significant impact on the surface energy and moisture balance, which play a key role in ecosystem diversity and productivity. The air-/space-borne Global Navigation Satellite System (GNSS)-Reflectometry (GNSS-R) is a bistatic radar with receiving power as the Delay Doppler Map (DDM), which may monitor soil freeze/thaw processes. However, the scattering mechanism of monitoring soil freeze/thaw processes by GNSS-R DDM is not clear. In this paper, it is the first time to simulate full-polarization GNSS-R Delay-Doppler-Map (DDM) for bare soil freeze/thaw process, not only the linear polarization but also the circular polarizations. As the bare soil freeze/thaw process occurs, the corresponding DDM variations are able to present by this simulator. Other geophysical parameters, such as soil moisture and surface roughness, are also two important parameters affecting the final GNSS-R receiver power and their effects on DDM are also presented by the simulator. This simulator can be a potentially efficient tool for data analysis and interoperation of GNSS-R received power as well as the in situ experimental design.http://link.springer.com/article/10.1186/s40562-020-00154-8GNSS-RDelay Doppler Map (DDM)Electromagnetic modelsFull polarizationsBare soil freeze/thaw process
collection DOAJ
language English
format Article
sources DOAJ
author Xuerui Wu
Shuanggen Jin
Xinqiu Ouyang
spellingShingle Xuerui Wu
Shuanggen Jin
Xinqiu Ouyang
A full-polarization GNSS-R Delay-Doppler-Map (DDM) simulator for bare soil freeze/thaw process detection
Geoscience Letters
GNSS-R
Delay Doppler Map (DDM)
Electromagnetic models
Full polarizations
Bare soil freeze/thaw process
author_facet Xuerui Wu
Shuanggen Jin
Xinqiu Ouyang
author_sort Xuerui Wu
title A full-polarization GNSS-R Delay-Doppler-Map (DDM) simulator for bare soil freeze/thaw process detection
title_short A full-polarization GNSS-R Delay-Doppler-Map (DDM) simulator for bare soil freeze/thaw process detection
title_full A full-polarization GNSS-R Delay-Doppler-Map (DDM) simulator for bare soil freeze/thaw process detection
title_fullStr A full-polarization GNSS-R Delay-Doppler-Map (DDM) simulator for bare soil freeze/thaw process detection
title_full_unstemmed A full-polarization GNSS-R Delay-Doppler-Map (DDM) simulator for bare soil freeze/thaw process detection
title_sort full-polarization gnss-r delay-doppler-map (ddm) simulator for bare soil freeze/thaw process detection
publisher SpringerOpen
series Geoscience Letters
issn 2196-4092
publishDate 2020-03-01
description Abstract The soil freeze/thaw processes have a significant impact on the surface energy and moisture balance, which play a key role in ecosystem diversity and productivity. The air-/space-borne Global Navigation Satellite System (GNSS)-Reflectometry (GNSS-R) is a bistatic radar with receiving power as the Delay Doppler Map (DDM), which may monitor soil freeze/thaw processes. However, the scattering mechanism of monitoring soil freeze/thaw processes by GNSS-R DDM is not clear. In this paper, it is the first time to simulate full-polarization GNSS-R Delay-Doppler-Map (DDM) for bare soil freeze/thaw process, not only the linear polarization but also the circular polarizations. As the bare soil freeze/thaw process occurs, the corresponding DDM variations are able to present by this simulator. Other geophysical parameters, such as soil moisture and surface roughness, are also two important parameters affecting the final GNSS-R receiver power and their effects on DDM are also presented by the simulator. This simulator can be a potentially efficient tool for data analysis and interoperation of GNSS-R received power as well as the in situ experimental design.
topic GNSS-R
Delay Doppler Map (DDM)
Electromagnetic models
Full polarizations
Bare soil freeze/thaw process
url http://link.springer.com/article/10.1186/s40562-020-00154-8
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