Geodesy for Essential Climate Variable products associated with Permafrost

Permafrost has long been listed as a terrestrial Essential Climate Variable (ECV) by the Global Climate Observing System (GSOS). According to the GSOS ECVs guidelines and requirements as released in 2022, three ECV products are associated with permafrost, including permafrost temperature, active lay...

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Main Author: Liu, L.
Format: Conference Object
Language:English
Published: 2023
Subjects:
Online Access:https://gfzpublic.gfz-potsdam.de/pubman/item/item_5017255
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spelling ftgfzpotsdam:oai:gfzpublic.gfz-potsdam.de:item_5017255 2023-10-01T03:49:40+02:00 Geodesy for Essential Climate Variable products associated with Permafrost Liu, L. 2023 https://gfzpublic.gfz-potsdam.de/pubman/item/item_5017255 eng eng info:eu-repo/semantics/altIdentifier/doi/10.57757/IUGG23-1340 https://gfzpublic.gfz-potsdam.de/pubman/item/item_5017255 XXVIII General Assembly of the International Union of Geodesy and Geophysics (IUGG) info:eu-repo/semantics/conferenceObject 2023 ftgfzpotsdam https://doi.org/10.57757/IUGG23-1340 2023-09-03T23:42:30Z Permafrost has long been listed as a terrestrial Essential Climate Variable (ECV) by the Global Climate Observing System (GSOS). According to the GSOS ECVs guidelines and requirements as released in 2022, three ECV products are associated with permafrost, including permafrost temperature, active layer thickness, and rock glacier velocity. Since permafrost is purely defined by the subsurface temperature, many of its changes occurring underground are mainly observed by borehole measurements but with limited spatial coverage. This paper reviews the applications and potential of geodetic methods to generate ECV products of active layer thickness and rock glacier velocity. Leveling, InSAR, and GNSS Interferometric Reflectometry measure seasonal, cyclic thaw subsidence and frost heave. A few retrieval algorithms have been developed to take the geodetic measurements of elevation changes as the input to indirectly estimate active layer thickness and have achieved moderate success in a few case studies. Substantial improvements, especially incorporation with frozen ground hydro-thermal models and remote sensing products of soil moisture and ground surface temperature, are warranted to improve the accuracy and generalizability of geodetic methods for generating reliable active layer thickness. Despite being just added by GSOS in 2022 as a new ECV product, rock glacier velocity has been routinely measured using various geodetic methods including theodolites, total stations, GNSS, laser scanning, and InSAR for years to decades. The geodesy community should be actively involved to provide inputs to the International Permafrost Association to standardize the measurement protocols for monitoring changes of rock glacier velocities around the globe. Conference Object Active layer thickness International Permafrost Association permafrost GFZpublic (German Research Centre for Geosciences, Helmholtz-Zentrum Potsdam)
institution Open Polar
collection GFZpublic (German Research Centre for Geosciences, Helmholtz-Zentrum Potsdam)
op_collection_id ftgfzpotsdam
language English
description Permafrost has long been listed as a terrestrial Essential Climate Variable (ECV) by the Global Climate Observing System (GSOS). According to the GSOS ECVs guidelines and requirements as released in 2022, three ECV products are associated with permafrost, including permafrost temperature, active layer thickness, and rock glacier velocity. Since permafrost is purely defined by the subsurface temperature, many of its changes occurring underground are mainly observed by borehole measurements but with limited spatial coverage. This paper reviews the applications and potential of geodetic methods to generate ECV products of active layer thickness and rock glacier velocity. Leveling, InSAR, and GNSS Interferometric Reflectometry measure seasonal, cyclic thaw subsidence and frost heave. A few retrieval algorithms have been developed to take the geodetic measurements of elevation changes as the input to indirectly estimate active layer thickness and have achieved moderate success in a few case studies. Substantial improvements, especially incorporation with frozen ground hydro-thermal models and remote sensing products of soil moisture and ground surface temperature, are warranted to improve the accuracy and generalizability of geodetic methods for generating reliable active layer thickness. Despite being just added by GSOS in 2022 as a new ECV product, rock glacier velocity has been routinely measured using various geodetic methods including theodolites, total stations, GNSS, laser scanning, and InSAR for years to decades. The geodesy community should be actively involved to provide inputs to the International Permafrost Association to standardize the measurement protocols for monitoring changes of rock glacier velocities around the globe.
format Conference Object
author Liu, L.
spellingShingle Liu, L.
Geodesy for Essential Climate Variable products associated with Permafrost
author_facet Liu, L.
author_sort Liu, L.
title Geodesy for Essential Climate Variable products associated with Permafrost
title_short Geodesy for Essential Climate Variable products associated with Permafrost
title_full Geodesy for Essential Climate Variable products associated with Permafrost
title_fullStr Geodesy for Essential Climate Variable products associated with Permafrost
title_full_unstemmed Geodesy for Essential Climate Variable products associated with Permafrost
title_sort geodesy for essential climate variable products associated with permafrost
publishDate 2023
url https://gfzpublic.gfz-potsdam.de/pubman/item/item_5017255
genre Active layer thickness
International Permafrost Association
permafrost
genre_facet Active layer thickness
International Permafrost Association
permafrost
op_source XXVIII General Assembly of the International Union of Geodesy and Geophysics (IUGG)
op_relation info:eu-repo/semantics/altIdentifier/doi/10.57757/IUGG23-1340
https://gfzpublic.gfz-potsdam.de/pubman/item/item_5017255
op_doi https://doi.org/10.57757/IUGG23-1340
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