Estimation of snow characteristics at the Polish Polar Station Hornsund, Svalbard, based on the GNSS-IR method

Information on snow depth and density is necessary for managing water supply in seasonal snow-covered regions. They are critical parameters in research topics such as hydrology and glaciology, especially concerning climate change. Unfortunately, regular observations of the snow cover in the High Arc...

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Main Authors: Grzymała, M., Prochniewicz, D., Luks, B.
Format: Conference Object
Language:English
Published: 2023
Subjects:
Online Access:https://gfzpublic.gfz-potsdam.de/pubman/item/item_5017700
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spelling ftgfzpotsdam:oai:gfzpublic.gfz-potsdam.de:item_5017700 2023-10-01T03:53:51+02:00 Estimation of snow characteristics at the Polish Polar Station Hornsund, Svalbard, based on the GNSS-IR method Grzymała, M. Prochniewicz, D. Luks, B. 2023 https://gfzpublic.gfz-potsdam.de/pubman/item/item_5017700 eng eng info:eu-repo/semantics/altIdentifier/doi/10.57757/IUGG23-1873 https://gfzpublic.gfz-potsdam.de/pubman/item/item_5017700 XXVIII General Assembly of the International Union of Geodesy and Geophysics (IUGG) info:eu-repo/semantics/conferenceObject 2023 ftgfzpotsdam https://doi.org/10.57757/IUGG23-1873 2023-09-03T23:42:28Z Information on snow depth and density is necessary for managing water supply in seasonal snow-covered regions. They are critical parameters in research topics such as hydrology and glaciology, especially concerning climate change. Unfortunately, regular observations of the snow cover in the High Arctic are challenging due to the high cost of manual measurements and it pointed character. The GNSS Interferometric Reflectometry (GNSS-IR) is a technique that allows the determination of many characteristics of the environment surrounding the measuring antenna. It is based on the frequency of the multipath-induced oscillations in the SNR parameters analysis, which vary depending on the surface cover. It makes the GNSS-IR method suitable in snow cover research, solving the issues of manual measurements since it is a mainly automated process with limited fieldwork and non-invasiveness. The contribution outlines the results, such as the snow depth of the surrounding area, obtained using GNSS-IR technique for Multi-GNSS observations, with its verification to the in-situ measurements. The observations from the GNSS-IR station installed as a realization of the Arctic Field Grant at the Polish Polar Station Hornsund, Svalbard, recorded during the annual snow period, are used in the work. This measurement site is the only operating GNSS-IR station in this part of Spitsbergen and is to become a part of the CRIOS infrastructure. Conference Object Arctic Climate change Hornsund Svalbard Spitsbergen GFZpublic (German Research Centre for Geosciences, Helmholtz-Zentrum Potsdam) Arctic Svalbard Hornsund ENVELOPE(15.865,15.865,76.979,76.979)
institution Open Polar
collection GFZpublic (German Research Centre for Geosciences, Helmholtz-Zentrum Potsdam)
op_collection_id ftgfzpotsdam
language English
description Information on snow depth and density is necessary for managing water supply in seasonal snow-covered regions. They are critical parameters in research topics such as hydrology and glaciology, especially concerning climate change. Unfortunately, regular observations of the snow cover in the High Arctic are challenging due to the high cost of manual measurements and it pointed character. The GNSS Interferometric Reflectometry (GNSS-IR) is a technique that allows the determination of many characteristics of the environment surrounding the measuring antenna. It is based on the frequency of the multipath-induced oscillations in the SNR parameters analysis, which vary depending on the surface cover. It makes the GNSS-IR method suitable in snow cover research, solving the issues of manual measurements since it is a mainly automated process with limited fieldwork and non-invasiveness. The contribution outlines the results, such as the snow depth of the surrounding area, obtained using GNSS-IR technique for Multi-GNSS observations, with its verification to the in-situ measurements. The observations from the GNSS-IR station installed as a realization of the Arctic Field Grant at the Polish Polar Station Hornsund, Svalbard, recorded during the annual snow period, are used in the work. This measurement site is the only operating GNSS-IR station in this part of Spitsbergen and is to become a part of the CRIOS infrastructure.
format Conference Object
author Grzymała, M.
Prochniewicz, D.
Luks, B.
spellingShingle Grzymała, M.
Prochniewicz, D.
Luks, B.
Estimation of snow characteristics at the Polish Polar Station Hornsund, Svalbard, based on the GNSS-IR method
author_facet Grzymała, M.
Prochniewicz, D.
Luks, B.
author_sort Grzymała, M.
title Estimation of snow characteristics at the Polish Polar Station Hornsund, Svalbard, based on the GNSS-IR method
title_short Estimation of snow characteristics at the Polish Polar Station Hornsund, Svalbard, based on the GNSS-IR method
title_full Estimation of snow characteristics at the Polish Polar Station Hornsund, Svalbard, based on the GNSS-IR method
title_fullStr Estimation of snow characteristics at the Polish Polar Station Hornsund, Svalbard, based on the GNSS-IR method
title_full_unstemmed Estimation of snow characteristics at the Polish Polar Station Hornsund, Svalbard, based on the GNSS-IR method
title_sort estimation of snow characteristics at the polish polar station hornsund, svalbard, based on the gnss-ir method
publishDate 2023
url https://gfzpublic.gfz-potsdam.de/pubman/item/item_5017700
long_lat ENVELOPE(15.865,15.865,76.979,76.979)
geographic Arctic
Svalbard
Hornsund
geographic_facet Arctic
Svalbard
Hornsund
genre Arctic
Climate change
Hornsund
Svalbard
Spitsbergen
genre_facet Arctic
Climate change
Hornsund
Svalbard
Spitsbergen
op_source XXVIII General Assembly of the International Union of Geodesy and Geophysics (IUGG)
op_relation info:eu-repo/semantics/altIdentifier/doi/10.57757/IUGG23-1873
https://gfzpublic.gfz-potsdam.de/pubman/item/item_5017700
op_doi https://doi.org/10.57757/IUGG23-1873
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