The Use of National CORS Networks for Determining Temporal Mass Variations within the Earth’s System and for Improving GRACE/GRACE-FO Solutions

Temporal mass variations within the Earth’s system can be detected on a regional/global scale using GRACE (Gravity Recovery and Climate Experiment) and GRACE Follow-On (GRACE-FO) satellite missions’ data, while GNSS (Global Navigation Satellite System) data can be used to detect those variations on...

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Main Authors: Walyeldeen Godah, Jagat Dwipendra Ray, Malgorzata Szelachowska, Jan Krynski
Format: Article
Language:English
Published: MDPI AG 2020-10-01
Series:Remote Sensing
Subjects:
Online Access:https://www.mdpi.com/2072-4292/12/20/3359
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author Walyeldeen Godah
Jagat Dwipendra Ray
Malgorzata Szelachowska
Jan Krynski
author_facet Walyeldeen Godah
Jagat Dwipendra Ray
Malgorzata Szelachowska
Jan Krynski
author_sort Walyeldeen Godah
collection DOAJ
description Temporal mass variations within the Earth’s system can be detected on a regional/global scale using GRACE (Gravity Recovery and Climate Experiment) and GRACE Follow-On (GRACE-FO) satellite missions’ data, while GNSS (Global Navigation Satellite System) data can be used to detect those variations on a local scale. The aim of this study is to investigate the usefulness of national GNSS CORS (Continuously Operating Reference Stations) networks for the determination of those temporal mass variations and for improving GRACE/GRACE-FO solutions. The area of Poland was chosen as a study area. Temporal variations of equivalent water thickness Δ<i>EWT</i> and vertical deformations of the Earth’s surface Δ<i>h</i> were determined at the sites of the ASG-EUPOS (Active Geodetic Network of the European Position Determination System) CORS network using GRACE/GRACE-FO-based GGMs and GNSS data. Moreover, combined solutions of Δ<i>EWT</i> were developed by combining Δ<i>EWT</i> obtained from GNSS data with the corresponding ones determined from GRACE satellite mission data. Strong correlations (correlation coefficients ranging from 0.6 to 0.9) between detrended Δ<i>h</i> determined from GRACE/GRACE-FO satellite mission data and the corresponding ones from GNSS data were observed at 93% of the GNSS stations investigated. Furthermore, for the determination of temporal mass variations, GNSS data from CORS network stations provide valuable information complementary to GRACE satellite mission data.
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spelling doaj.art-551a4208515143c1a0a5eb7ad4c35d9f2023-11-20T17:15:16ZengMDPI AGRemote Sensing2072-42922020-10-011220335910.3390/rs12203359The Use of National CORS Networks for Determining Temporal Mass Variations within the Earth’s System and for Improving GRACE/GRACE-FO SolutionsWalyeldeen Godah0Jagat Dwipendra Ray1Malgorzata Szelachowska2Jan Krynski3Institute of Geodesy and Cartography, Centre of Geodesy and Geodynamics, 27 Modzelewskiego St., 02-679 Warsaw, PolandInstitute of Geodesy and Cartography, Centre of Geodesy and Geodynamics, 27 Modzelewskiego St., 02-679 Warsaw, PolandInstitute of Geodesy and Cartography, Centre of Geodesy and Geodynamics, 27 Modzelewskiego St., 02-679 Warsaw, PolandInstitute of Geodesy and Cartography, Centre of Geodesy and Geodynamics, 27 Modzelewskiego St., 02-679 Warsaw, PolandTemporal mass variations within the Earth’s system can be detected on a regional/global scale using GRACE (Gravity Recovery and Climate Experiment) and GRACE Follow-On (GRACE-FO) satellite missions’ data, while GNSS (Global Navigation Satellite System) data can be used to detect those variations on a local scale. The aim of this study is to investigate the usefulness of national GNSS CORS (Continuously Operating Reference Stations) networks for the determination of those temporal mass variations and for improving GRACE/GRACE-FO solutions. The area of Poland was chosen as a study area. Temporal variations of equivalent water thickness Δ<i>EWT</i> and vertical deformations of the Earth’s surface Δ<i>h</i> were determined at the sites of the ASG-EUPOS (Active Geodetic Network of the European Position Determination System) CORS network using GRACE/GRACE-FO-based GGMs and GNSS data. Moreover, combined solutions of Δ<i>EWT</i> were developed by combining Δ<i>EWT</i> obtained from GNSS data with the corresponding ones determined from GRACE satellite mission data. Strong correlations (correlation coefficients ranging from 0.6 to 0.9) between detrended Δ<i>h</i> determined from GRACE/GRACE-FO satellite mission data and the corresponding ones from GNSS data were observed at 93% of the GNSS stations investigated. Furthermore, for the determination of temporal mass variations, GNSS data from CORS network stations provide valuable information complementary to GRACE satellite mission data.https://www.mdpi.com/2072-4292/12/20/3359equivalent water thicknessGNSSGRACE/GRACE-FOtemporal mass variations within the Earth’s systemvertical surface deformation
spellingShingle Walyeldeen Godah
Jagat Dwipendra Ray
Malgorzata Szelachowska
Jan Krynski
The Use of National CORS Networks for Determining Temporal Mass Variations within the Earth’s System and for Improving GRACE/GRACE-FO Solutions
Remote Sensing
equivalent water thickness
GNSS
GRACE/GRACE-FO
temporal mass variations within the Earth’s system
vertical surface deformation
title The Use of National CORS Networks for Determining Temporal Mass Variations within the Earth’s System and for Improving GRACE/GRACE-FO Solutions
title_full The Use of National CORS Networks for Determining Temporal Mass Variations within the Earth’s System and for Improving GRACE/GRACE-FO Solutions
title_fullStr The Use of National CORS Networks for Determining Temporal Mass Variations within the Earth’s System and for Improving GRACE/GRACE-FO Solutions
title_full_unstemmed The Use of National CORS Networks for Determining Temporal Mass Variations within the Earth’s System and for Improving GRACE/GRACE-FO Solutions
title_short The Use of National CORS Networks for Determining Temporal Mass Variations within the Earth’s System and for Improving GRACE/GRACE-FO Solutions
title_sort use of national cors networks for determining temporal mass variations within the earth s system and for improving grace grace fo solutions
topic equivalent water thickness
GNSS
GRACE/GRACE-FO
temporal mass variations within the Earth’s system
vertical surface deformation
url https://www.mdpi.com/2072-4292/12/20/3359
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