Glacial and erosional contributions to Late Quaternary uplift of the European Alps (GEOLQUEA) ...

Isostatic adjustments of the Earth’s surface to changes in water, ice, and sediment loading are important contributions to present-day uplift/subsidence rates in many regions on Earth. In the absence of significant horizontal tectonic shortening in the central and western parts of the European Alps,...

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Main Authors: Scherler, Dirk, Werner, Helen, Winkelmann, Ricarda, Jouvet, Guillaume, Klemann, Volker
Format: Text
Language:unknown
Published: Freie Universität Berlin 2023
Subjects:
Online Access:https://dx.doi.org/10.17169/refubium-41081
https://refubium.fu-berlin.de/handle/fub188/41360
id ftdatacite:10.17169/refubium-41081
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spelling ftdatacite:10.17169/refubium-41081 2023-12-31T10:08:00+01:00 Glacial and erosional contributions to Late Quaternary uplift of the European Alps (GEOLQUEA) ... Scherler, Dirk Werner, Helen Winkelmann, Ricarda Jouvet, Guillaume Klemann, Volker 2023 https://dx.doi.org/10.17169/refubium-41081 https://refubium.fu-berlin.de/handle/fub188/41360 unknown Freie Universität Berlin http://www.spp-mountainbuilding.de/events/AA-4DMB_annual_meeting_BadHofgastein_2023.html Creative Commons Attribution 4.0 International https://creativecommons.org/licenses/by/4.0/legalcode cc-by-4.0 Ice sheet modelling Late Quaternary uplift European Alps 500 Natural sciences and mathematics550 Earth sciences550 Earth sciences ScholarlyArticle Abstract article-journal Text 2023 ftdatacite https://doi.org/10.17169/refubium-41081 2023-12-01T10:29:53Z Isostatic adjustments of the Earth’s surface to changes in water, ice, and sediment loading are important contributions to present-day uplift/subsidence rates in many regions on Earth. In the absence of significant horizontal tectonic shortening in the central and western parts of the European Alps, uplift rates larger than 2 mm/yr are difficult to explain by geodynamic processes and have been a matter of debate for many decades. Here we examine the likely contribution of glacial isostatic adjustment in the European Alps in response to changes in ice loading using state of the art ice flow and lithospheric numerical modeling. In contrast to a similar previous approach (Mey et al., 2016), we employ a transient ice sheet model over the last glacial cycle (100 kyr) in combination with a spherical viscoelastic solid earth model. We present ice model results using the Instructed Glacier Model (Jouvet et al., 2021), in which we tested the effect of spatial resolution on the growth and extent of the European ice ... Text Ice Sheet DataCite Metadata Store (German National Library of Science and Technology)
institution Open Polar
collection DataCite Metadata Store (German National Library of Science and Technology)
op_collection_id ftdatacite
language unknown
topic Ice sheet modelling
Late Quaternary uplift
European Alps
500 Natural sciences and mathematics550 Earth sciences550 Earth sciences
spellingShingle Ice sheet modelling
Late Quaternary uplift
European Alps
500 Natural sciences and mathematics550 Earth sciences550 Earth sciences
Scherler, Dirk
Werner, Helen
Winkelmann, Ricarda
Jouvet, Guillaume
Klemann, Volker
Glacial and erosional contributions to Late Quaternary uplift of the European Alps (GEOLQUEA) ...
topic_facet Ice sheet modelling
Late Quaternary uplift
European Alps
500 Natural sciences and mathematics550 Earth sciences550 Earth sciences
description Isostatic adjustments of the Earth’s surface to changes in water, ice, and sediment loading are important contributions to present-day uplift/subsidence rates in many regions on Earth. In the absence of significant horizontal tectonic shortening in the central and western parts of the European Alps, uplift rates larger than 2 mm/yr are difficult to explain by geodynamic processes and have been a matter of debate for many decades. Here we examine the likely contribution of glacial isostatic adjustment in the European Alps in response to changes in ice loading using state of the art ice flow and lithospheric numerical modeling. In contrast to a similar previous approach (Mey et al., 2016), we employ a transient ice sheet model over the last glacial cycle (100 kyr) in combination with a spherical viscoelastic solid earth model. We present ice model results using the Instructed Glacier Model (Jouvet et al., 2021), in which we tested the effect of spatial resolution on the growth and extent of the European ice ...
format Text
author Scherler, Dirk
Werner, Helen
Winkelmann, Ricarda
Jouvet, Guillaume
Klemann, Volker
author_facet Scherler, Dirk
Werner, Helen
Winkelmann, Ricarda
Jouvet, Guillaume
Klemann, Volker
author_sort Scherler, Dirk
title Glacial and erosional contributions to Late Quaternary uplift of the European Alps (GEOLQUEA) ...
title_short Glacial and erosional contributions to Late Quaternary uplift of the European Alps (GEOLQUEA) ...
title_full Glacial and erosional contributions to Late Quaternary uplift of the European Alps (GEOLQUEA) ...
title_fullStr Glacial and erosional contributions to Late Quaternary uplift of the European Alps (GEOLQUEA) ...
title_full_unstemmed Glacial and erosional contributions to Late Quaternary uplift of the European Alps (GEOLQUEA) ...
title_sort glacial and erosional contributions to late quaternary uplift of the european alps (geolquea) ...
publisher Freie Universität Berlin
publishDate 2023
url https://dx.doi.org/10.17169/refubium-41081
https://refubium.fu-berlin.de/handle/fub188/41360
genre Ice Sheet
genre_facet Ice Sheet
op_relation http://www.spp-mountainbuilding.de/events/AA-4DMB_annual_meeting_BadHofgastein_2023.html
op_rights Creative Commons Attribution 4.0 International
https://creativecommons.org/licenses/by/4.0/legalcode
cc-by-4.0
op_doi https://doi.org/10.17169/refubium-41081
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