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record_format openpolar
spelling ftunigrenoble:oai:HAL:tel-01760438v1 2024-05-12T07:55:54+00:00 Ocean / Ice sheet interactions : toward a coupled model system Interactions calotte polaire/océan : vers la mise en place d'une modélisation couplée Merino, Nacho Institut des Géosciences de l’Environnement (IGE) Institut de Recherche pour le Développement (IRD)-Institut polytechnique de Grenoble - Grenoble Institute of Technology (Grenoble INP )-Institut national des sciences de l'Univers (INSU - CNRS)-Centre National de la Recherche Scientifique (CNRS)-Université Grenoble Alpes 2016-2019 (UGA 2016-2019 ) Université Grenoble Alpes Gaël Durand Julien Le Sommer 2016-12-02 https://theses.hal.science/tel-01760438 https://theses.hal.science/tel-01760438/document https://theses.hal.science/tel-01760438/file/MERINO_2016_archivage.pdf en eng HAL CCSD NNT: 2016GREAU051 tel-01760438 https://theses.hal.science/tel-01760438 https://theses.hal.science/tel-01760438/document https://theses.hal.science/tel-01760438/file/MERINO_2016_archivage.pdf info:eu-repo/semantics/OpenAccess https://theses.hal.science/tel-01760438 Glaciology. Université Grenoble Alpes, 2016. English. ⟨NNT : 2016GREAU051⟩ Ice sheet Ocean Model Icebergs Calotte polaire Océan Modèle [SDU.STU.GL]Sciences of the Universe [physics]/Earth Sciences/Glaciology [SDU.STU.OC]Sciences of the Universe [physics]/Earth Sciences/Oceanography info:eu-repo/semantics/doctoralThesis Theses 2016 ftunigrenoble 2024-04-18T03:59:18Z The next generation of climate models will include an ice-sheet model in order to improve the ice sheet mass balance projections by accounting for the ice dynamics and ice-oceans interactions. On the one hand, the Southern Ocean (SO) is indeed driving the acceleration of the Antarctic outlet glaciers via an increase in the basal melting of the ice shelves. On the other hand, the increasing ice discharge from Antarctic Ice Sheet (AIS) contributes to the current sea level rise and is likely to become the largest cryospheric contributor to sea level rise by the end of the current century. In addition, the related freshening may have significant implications on future sea-ice cover and on bottom water formation. However, it is not clear yet how the ocean and ice-sheet components of future coupled systems will account for the ice-ocean interactions, which are both causes and consequences of the AIS mass imbalance. Here in this work, different aspects of the standalone ocean and ice-sheet components have been investigated. A first step of this thesis has been focused in the representation of the glacial freshwater fluxes in current ocean models. Based on recent glaciological estimates, the ice shelf basal melting fluxes have been spatially distributed in an ORCA025 grid, and the calving rates have been applied into an improved version of the NEMO-ICB iceberg model. This preliminary study has been used to produce a monthly iceberg meltwater climatology, to be used to force current ocean models. This work shows the importance of representing the iceberg meltwater fluxes when modeling sea ice, which can be inexpensively achieve by using our climatology. The improvements in the representation of the glacial freshwater fluxes have been considered in the study of the ocean model response to the Antarctic mass imbalance. This study considers a realistic perturbation in the glacial freshwater forcing as close as possible as it will be represented in future ice-sheet/ocean models. According to our results, up to 50% of the ... Doctoral or Postdoctoral Thesis Antarc* Antarctic Ice Sheet Ice Shelf Ice Shelves Iceberg* Sea ice Southern Ocean Université Grenoble Alpes: HAL Antarctic Southern Ocean The Antarctic
institution Open Polar
collection Université Grenoble Alpes: HAL
op_collection_id ftunigrenoble
language English
topic Ice sheet
Ocean
Model
Icebergs
Calotte polaire
Océan
Modèle
[SDU.STU.GL]Sciences of the Universe [physics]/Earth Sciences/Glaciology
[SDU.STU.OC]Sciences of the Universe [physics]/Earth Sciences/Oceanography
spellingShingle Ice sheet
Ocean
Model
Icebergs
Calotte polaire
Océan
Modèle
[SDU.STU.GL]Sciences of the Universe [physics]/Earth Sciences/Glaciology
[SDU.STU.OC]Sciences of the Universe [physics]/Earth Sciences/Oceanography
Merino, Nacho
Ocean / Ice sheet interactions : toward a coupled model system
topic_facet Ice sheet
Ocean
Model
Icebergs
Calotte polaire
Océan
Modèle
[SDU.STU.GL]Sciences of the Universe [physics]/Earth Sciences/Glaciology
[SDU.STU.OC]Sciences of the Universe [physics]/Earth Sciences/Oceanography
description The next generation of climate models will include an ice-sheet model in order to improve the ice sheet mass balance projections by accounting for the ice dynamics and ice-oceans interactions. On the one hand, the Southern Ocean (SO) is indeed driving the acceleration of the Antarctic outlet glaciers via an increase in the basal melting of the ice shelves. On the other hand, the increasing ice discharge from Antarctic Ice Sheet (AIS) contributes to the current sea level rise and is likely to become the largest cryospheric contributor to sea level rise by the end of the current century. In addition, the related freshening may have significant implications on future sea-ice cover and on bottom water formation. However, it is not clear yet how the ocean and ice-sheet components of future coupled systems will account for the ice-ocean interactions, which are both causes and consequences of the AIS mass imbalance. Here in this work, different aspects of the standalone ocean and ice-sheet components have been investigated. A first step of this thesis has been focused in the representation of the glacial freshwater fluxes in current ocean models. Based on recent glaciological estimates, the ice shelf basal melting fluxes have been spatially distributed in an ORCA025 grid, and the calving rates have been applied into an improved version of the NEMO-ICB iceberg model. This preliminary study has been used to produce a monthly iceberg meltwater climatology, to be used to force current ocean models. This work shows the importance of representing the iceberg meltwater fluxes when modeling sea ice, which can be inexpensively achieve by using our climatology. The improvements in the representation of the glacial freshwater fluxes have been considered in the study of the ocean model response to the Antarctic mass imbalance. This study considers a realistic perturbation in the glacial freshwater forcing as close as possible as it will be represented in future ice-sheet/ocean models. According to our results, up to 50% of the ...
author2 Institut des Géosciences de l’Environnement (IGE)
Institut de Recherche pour le Développement (IRD)-Institut polytechnique de Grenoble - Grenoble Institute of Technology (Grenoble INP )-Institut national des sciences de l'Univers (INSU - CNRS)-Centre National de la Recherche Scientifique (CNRS)-Université Grenoble Alpes 2016-2019 (UGA 2016-2019 )
Université Grenoble Alpes
Gaël Durand
Julien Le Sommer
format Doctoral or Postdoctoral Thesis
author Merino, Nacho
author_facet Merino, Nacho
author_sort Merino, Nacho
title Ocean / Ice sheet interactions : toward a coupled model system
title_short Ocean / Ice sheet interactions : toward a coupled model system
title_full Ocean / Ice sheet interactions : toward a coupled model system
title_fullStr Ocean / Ice sheet interactions : toward a coupled model system
title_full_unstemmed Ocean / Ice sheet interactions : toward a coupled model system
title_sort ocean / ice sheet interactions : toward a coupled model system
publisher HAL CCSD
publishDate 2016
url https://theses.hal.science/tel-01760438
https://theses.hal.science/tel-01760438/document
https://theses.hal.science/tel-01760438/file/MERINO_2016_archivage.pdf
geographic Antarctic
Southern Ocean
The Antarctic
geographic_facet Antarctic
Southern Ocean
The Antarctic
genre Antarc*
Antarctic
Ice Sheet
Ice Shelf
Ice Shelves
Iceberg*
Sea ice
Southern Ocean
genre_facet Antarc*
Antarctic
Ice Sheet
Ice Shelf
Ice Shelves
Iceberg*
Sea ice
Southern Ocean
op_source https://theses.hal.science/tel-01760438
Glaciology. Université Grenoble Alpes, 2016. English. ⟨NNT : 2016GREAU051⟩
op_relation NNT: 2016GREAU051
tel-01760438
https://theses.hal.science/tel-01760438
https://theses.hal.science/tel-01760438/document
https://theses.hal.science/tel-01760438/file/MERINO_2016_archivage.pdf
op_rights info:eu-repo/semantics/OpenAccess
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