Coastal change in a warming Arctic

International audience The coastline of Svalbard is highly dynamic. Coastal erosion, delta progradation, longshore drift and spit migration are parts of the Svalbard coastal environment and contribute to bathymetry changes, risk for infrastructure and cultural heritage, sediment budgets and nutrient...

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Main Authors: Jensen, Maria, Rubensdotter, Lena, Baltzer, Agnès, Choi, Kyungsik, Garestier, Franck
Other Authors: The University Centre in Svalbard (UNIS), Morphodynamique Continentale et Côtière (M2C), Université de Caen Normandie (UNICAEN), Normandie Université (NU)-Normandie Université (NU)-Institut national des sciences de l'Univers (INSU - CNRS)-Université de Rouen Normandie (UNIROUEN), Normandie Université (NU)-Centre National de la Recherche Scientifique (CNRS)
Format: Conference Object
Language:English
Published: HAL CCSD 2019
Subjects:
Ice
Online Access:https://hal.science/hal-02441434
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spelling ftinsu:oai:HAL:hal-02441434v1 2024-04-14T08:00:17+00:00 Coastal change in a warming Arctic Jensen, Maria Rubensdotter, Lena Baltzer, Agnès Choi, Kyungsik Garestier, Franck The University Centre in Svalbard (UNIS) Morphodynamique Continentale et Côtière (M2C) Université de Caen Normandie (UNICAEN) Normandie Université (NU)-Normandie Université (NU)-Institut national des sciences de l'Univers (INSU - CNRS)-Université de Rouen Normandie (UNIROUEN) Normandie Université (NU)-Centre National de la Recherche Scientifique (CNRS) Oslo, Norway 2019-11-05 https://hal.science/hal-02441434 en eng HAL CCSD hal-02441434 https://hal.science/hal-02441434 Svalbard Science Conference https://hal.science/hal-02441434 Svalbard Science Conference, Nov 2019, Oslo, Norway [SDE]Environmental Sciences info:eu-repo/semantics/conferenceObject Conference papers 2019 ftinsu 2024-03-21T17:20:01Z International audience The coastline of Svalbard is highly dynamic. Coastal erosion, delta progradation, longshore drift and spit migration are parts of the Svalbard coastal environment and contribute to bathymetry changes, risk for infrastructure and cultural heritage, sediment budgets and nutrient fluxes to fjord ecosystems. Hydrological change, permafrost degradation and increased slope instability change rates and sources of sediment supply from land to the coast. Changes in sea ice cover and wave activity affects the distribution of sediment from land to the sea. Until recently no quantification for change existed for the vast majority of the Svalbard coastline. Since 2017 baseline data for the coastal configuration in Isfjorden has been collected, which can now be combined with studies of coastal change on an annual to decadal time scale at representative sites in the Svalbard fjords. The aim of the studies are to quantify coastal change, understand the sediment delivery routes to the coast in different settings and understand the effect of open water for a significant part of the year/all year. This allows us to better predict coastal change both close to settlements and in remote parts of the archipelago, which is relevant for environmental and cultural heritage management. It also provides data on coastal sediment storage and release with implications for nutrient fluxes for marine ecosystem studies as well as for earth system models. We present the ongoing coastal mapping project of Isfjorden (DynaCoast) and the follow up remote sensing project MovingCoasts using SAR images to track high resolution coastal change. We also present close-up examples from the ongoing monitoring of coastal change in Kongsfjorden, Dicksonfjorden, Adventfjorden and Braganzavågen, and discuss how different settings are expected to respond differently to a warming climate scenario. Conference Object Adventfjorden Arctic Ice Isfjord* Isfjorden Kongsfjord* Kongsfjorden permafrost Sea ice Svalbard Institut national des sciences de l'Univers: HAL-INSU Arctic Svalbard Norway Adventfjorden ENVELOPE(15.515,15.515,78.258,78.258) Dicksonfjorden ENVELOPE(15.291,15.291,78.710,78.710) Braganzavågen ENVELOPE(16.864,16.864,77.894,77.894)
institution Open Polar
collection Institut national des sciences de l'Univers: HAL-INSU
op_collection_id ftinsu
language English
topic [SDE]Environmental Sciences
spellingShingle [SDE]Environmental Sciences
Jensen, Maria
Rubensdotter, Lena
Baltzer, Agnès
Choi, Kyungsik
Garestier, Franck
Coastal change in a warming Arctic
topic_facet [SDE]Environmental Sciences
description International audience The coastline of Svalbard is highly dynamic. Coastal erosion, delta progradation, longshore drift and spit migration are parts of the Svalbard coastal environment and contribute to bathymetry changes, risk for infrastructure and cultural heritage, sediment budgets and nutrient fluxes to fjord ecosystems. Hydrological change, permafrost degradation and increased slope instability change rates and sources of sediment supply from land to the coast. Changes in sea ice cover and wave activity affects the distribution of sediment from land to the sea. Until recently no quantification for change existed for the vast majority of the Svalbard coastline. Since 2017 baseline data for the coastal configuration in Isfjorden has been collected, which can now be combined with studies of coastal change on an annual to decadal time scale at representative sites in the Svalbard fjords. The aim of the studies are to quantify coastal change, understand the sediment delivery routes to the coast in different settings and understand the effect of open water for a significant part of the year/all year. This allows us to better predict coastal change both close to settlements and in remote parts of the archipelago, which is relevant for environmental and cultural heritage management. It also provides data on coastal sediment storage and release with implications for nutrient fluxes for marine ecosystem studies as well as for earth system models. We present the ongoing coastal mapping project of Isfjorden (DynaCoast) and the follow up remote sensing project MovingCoasts using SAR images to track high resolution coastal change. We also present close-up examples from the ongoing monitoring of coastal change in Kongsfjorden, Dicksonfjorden, Adventfjorden and Braganzavågen, and discuss how different settings are expected to respond differently to a warming climate scenario.
author2 The University Centre in Svalbard (UNIS)
Morphodynamique Continentale et Côtière (M2C)
Université de Caen Normandie (UNICAEN)
Normandie Université (NU)-Normandie Université (NU)-Institut national des sciences de l'Univers (INSU - CNRS)-Université de Rouen Normandie (UNIROUEN)
Normandie Université (NU)-Centre National de la Recherche Scientifique (CNRS)
format Conference Object
author Jensen, Maria
Rubensdotter, Lena
Baltzer, Agnès
Choi, Kyungsik
Garestier, Franck
author_facet Jensen, Maria
Rubensdotter, Lena
Baltzer, Agnès
Choi, Kyungsik
Garestier, Franck
author_sort Jensen, Maria
title Coastal change in a warming Arctic
title_short Coastal change in a warming Arctic
title_full Coastal change in a warming Arctic
title_fullStr Coastal change in a warming Arctic
title_full_unstemmed Coastal change in a warming Arctic
title_sort coastal change in a warming arctic
publisher HAL CCSD
publishDate 2019
url https://hal.science/hal-02441434
op_coverage Oslo, Norway
long_lat ENVELOPE(15.515,15.515,78.258,78.258)
ENVELOPE(15.291,15.291,78.710,78.710)
ENVELOPE(16.864,16.864,77.894,77.894)
geographic Arctic
Svalbard
Norway
Adventfjorden
Dicksonfjorden
Braganzavågen
geographic_facet Arctic
Svalbard
Norway
Adventfjorden
Dicksonfjorden
Braganzavågen
genre Adventfjorden
Arctic
Ice
Isfjord*
Isfjorden
Kongsfjord*
Kongsfjorden
permafrost
Sea ice
Svalbard
genre_facet Adventfjorden
Arctic
Ice
Isfjord*
Isfjorden
Kongsfjord*
Kongsfjorden
permafrost
Sea ice
Svalbard
op_source Svalbard Science Conference
https://hal.science/hal-02441434
Svalbard Science Conference, Nov 2019, Oslo, Norway
op_relation hal-02441434
https://hal.science/hal-02441434
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