Analytical Computation of the Spatial Resolution in GNSS-R and Experimental Validation at L1 and L5

Global navigation satellite systems reflectometry (GNSS-R) is a relatively novel remote sensing technique, but it can be understood as a multi-static radar using satellite navigation signals as signals of opportunity. The scattered signals over sea ice, flooded areas, and even under dense vegetation...

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Published in:Remote Sensing
Main Authors: Adriano Camps, Joan Francesc Munoz-Martin
Format: Text
Language:English
Published: Multidisciplinary Digital Publishing Institute 2020
Subjects:
L1
L5
Online Access:https://doi.org/10.3390/rs12233910
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spelling ftmdpi:oai:mdpi.com:/2072-4292/12/23/3910/ 2023-08-20T04:09:45+02:00 Analytical Computation of the Spatial Resolution in GNSS-R and Experimental Validation at L1 and L5 Adriano Camps Joan Francesc Munoz-Martin agris 2020-11-28 application/pdf https://doi.org/10.3390/rs12233910 EN eng Multidisciplinary Digital Publishing Institute https://dx.doi.org/10.3390/rs12233910 https://creativecommons.org/licenses/by/4.0/ Remote Sensing; Volume 12; Issue 23; Pages: 3910 GNSS-R spatial resolution diffraction experiment airborne L1 L5 Text 2020 ftmdpi https://doi.org/10.3390/rs12233910 2023-08-01T00:33:11Z Global navigation satellite systems reflectometry (GNSS-R) is a relatively novel remote sensing technique, but it can be understood as a multi-static radar using satellite navigation signals as signals of opportunity. The scattered signals over sea ice, flooded areas, and even under dense vegetation show a detectable coherent component that can be separated from the incoherent component and processed accordingly. This work derives an analytical formulation of the response of a GNSS-R instrument to a step function in the reflectivity using well-known principles of electromagnetic theory. The evaluation of the spatial resolution then requires a numerical evaluation of the proposed equations, as the width of the transition depends on the reflectivity values of two regions. However, it is found that results are fairly constant over a wide range of reflectivities, and they only vary faster for very high or very low reflectivity gradients. The predicted step response is then satisfactorily compared to airborne experimental results at L1 (1575.42 MHz) and L5 (1176.45 MHz) bands, acquired over a water reservoir south of Melbourne, in terms of width and ringing, and several examples are provided when the transition occurs from land to a rough ocean surface, where the coherent scattering component is no longer dominant. Text Sea ice MDPI Open Access Publishing Remote Sensing 12 23 3910
institution Open Polar
collection MDPI Open Access Publishing
op_collection_id ftmdpi
language English
topic GNSS-R
spatial resolution
diffraction
experiment
airborne
L1
L5
spellingShingle GNSS-R
spatial resolution
diffraction
experiment
airborne
L1
L5
Adriano Camps
Joan Francesc Munoz-Martin
Analytical Computation of the Spatial Resolution in GNSS-R and Experimental Validation at L1 and L5
topic_facet GNSS-R
spatial resolution
diffraction
experiment
airborne
L1
L5
description Global navigation satellite systems reflectometry (GNSS-R) is a relatively novel remote sensing technique, but it can be understood as a multi-static radar using satellite navigation signals as signals of opportunity. The scattered signals over sea ice, flooded areas, and even under dense vegetation show a detectable coherent component that can be separated from the incoherent component and processed accordingly. This work derives an analytical formulation of the response of a GNSS-R instrument to a step function in the reflectivity using well-known principles of electromagnetic theory. The evaluation of the spatial resolution then requires a numerical evaluation of the proposed equations, as the width of the transition depends on the reflectivity values of two regions. However, it is found that results are fairly constant over a wide range of reflectivities, and they only vary faster for very high or very low reflectivity gradients. The predicted step response is then satisfactorily compared to airborne experimental results at L1 (1575.42 MHz) and L5 (1176.45 MHz) bands, acquired over a water reservoir south of Melbourne, in terms of width and ringing, and several examples are provided when the transition occurs from land to a rough ocean surface, where the coherent scattering component is no longer dominant.
format Text
author Adriano Camps
Joan Francesc Munoz-Martin
author_facet Adriano Camps
Joan Francesc Munoz-Martin
author_sort Adriano Camps
title Analytical Computation of the Spatial Resolution in GNSS-R and Experimental Validation at L1 and L5
title_short Analytical Computation of the Spatial Resolution in GNSS-R and Experimental Validation at L1 and L5
title_full Analytical Computation of the Spatial Resolution in GNSS-R and Experimental Validation at L1 and L5
title_fullStr Analytical Computation of the Spatial Resolution in GNSS-R and Experimental Validation at L1 and L5
title_full_unstemmed Analytical Computation of the Spatial Resolution in GNSS-R and Experimental Validation at L1 and L5
title_sort analytical computation of the spatial resolution in gnss-r and experimental validation at l1 and l5
publisher Multidisciplinary Digital Publishing Institute
publishDate 2020
url https://doi.org/10.3390/rs12233910
op_coverage agris
genre Sea ice
genre_facet Sea ice
op_source Remote Sensing; Volume 12; Issue 23; Pages: 3910
op_relation https://dx.doi.org/10.3390/rs12233910
op_rights https://creativecommons.org/licenses/by/4.0/
op_doi https://doi.org/10.3390/rs12233910
container_title Remote Sensing
container_volume 12
container_issue 23
container_start_page 3910
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