Predominant Sea Ice Fracture Zones Around Antarctica and Their Relation to Bathymetric Features

International audience Sea ice is of substantial importance for the Southern Ocean, as it insulates the relatively warm ocean from the cold atmosphere. Due to mechanical stress induced by wind and ocean currents, sea ice leads occur, which are characterized by open water and thin ice causing an incr...

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Published in:Geophysical Research Letters
Main Authors: Reiser, F., Willmes, S., Hausmann, Ute, Heinemann, G.
Other Authors: Trier University, Laboratoire d'Océanographie et du Climat : Expérimentations et Approches Numériques (LOCEAN), Muséum national d'Histoire naturelle (MNHN)-Institut de Recherche pour le Développement (IRD)-Institut national des sciences de l'Univers (INSU - CNRS)-Sorbonne Université (SU)-Centre National de la Recherche Scientifique (CNRS)-Institut Pierre-Simon-Laplace (IPSL (FR_636)), École normale supérieure - Paris (ENS-PSL), Université Paris sciences et lettres (PSL)-Université Paris sciences et lettres (PSL)-Université de Versailles Saint-Quentin-en-Yvelines (UVSQ)-Commissariat à l'énergie atomique et aux énergies alternatives (CEA)-Institut national des sciences de l'Univers (INSU - CNRS)-École polytechnique (X)-Centre National d'Études Spatiales Toulouse (CNES)-Sorbonne Université (SU)-Centre National de la Recherche Scientifique (CNRS)-Université Paris Cité (UPCité)-École normale supérieure - Paris (ENS-PSL), Université Paris sciences et lettres (PSL)-Université Paris sciences et lettres (PSL)-Université de Versailles Saint-Quentin-en-Yvelines (UVSQ)-Commissariat à l'énergie atomique et aux énergies alternatives (CEA)-École polytechnique (X)-Centre National d'Études Spatiales Toulouse (CNES)-Sorbonne Université (SU)-Centre National de la Recherche Scientifique (CNRS)-Université Paris Cité (UPCité), European Project: 637770,H2020,ERC-2014-STG,WAPITI(2015)
Format: Article in Journal/Newspaper
Language:English
Published: HAL CCSD 2019
Subjects:
Online Access:https://hal.sorbonne-universite.fr/hal-02402416
https://hal.sorbonne-universite.fr/hal-02402416/document
https://hal.sorbonne-universite.fr/hal-02402416/file/Reiser_et_al-2019-Geophysical_Research_Letters.pdf
https://doi.org/10.1029/2019GL084624
id ftinsu:oai:HAL:hal-02402416v1
record_format openpolar
institution Open Polar
collection Institut national des sciences de l'Univers: HAL-INSU
op_collection_id ftinsu
language English
topic tides
ocean currents
bathymetry
MODIS
Antarctic sea ice leads
[SDU.STU.OC]Sciences of the Universe [physics]/Earth Sciences/Oceanography
spellingShingle tides
ocean currents
bathymetry
MODIS
Antarctic sea ice leads
[SDU.STU.OC]Sciences of the Universe [physics]/Earth Sciences/Oceanography
Reiser, F.
Willmes, S.
Hausmann, Ute
Heinemann, G.
Predominant Sea Ice Fracture Zones Around Antarctica and Their Relation to Bathymetric Features
topic_facet tides
ocean currents
bathymetry
MODIS
Antarctic sea ice leads
[SDU.STU.OC]Sciences of the Universe [physics]/Earth Sciences/Oceanography
description International audience Sea ice is of substantial importance for the Southern Ocean, as it insulates the relatively warm ocean from the cold atmosphere. Due to mechanical stress induced by wind and ocean currents, sea ice leads occur, which are characterized by open water and thin ice causing an increase of energy and moisture fluxes between ocean and atmosphere. Furthermore, they contribute to the ice production and provide a habitat for animals. Thus, it is important to gain information about the temporal and spatial distribution of leads on a circum-Antarctic scale. So far, no operational data set exists, which provides such information. We use thermal satellite imagery from the Moderate Resolution Imaging Spectroradiometer to derive the predominant lead patterns for 2003-2018, April-September. This study provides first results for the long-term average lead frequencies in the Southern Ocean and discusses possible links to ocean currents, tides, and the bathymetry. Plain Language Summary The polar regions are strongly influenced by sea ice, which covers large areas of the ocean's surface. Interacting with the atmosphere and the ocean, sea ice is a very dynamic surface with a large temporal and spatial variability. Under the forcing of winds and ocean currents, sea ice is subject to deformation processes causing cracks (leads) in the ice. The observation of these leads is the aim of this study since they are an important feature. For instance, open water can be found in these cracks, which enables the warm ocean (−1.7 • C) to lose energy to the cold atmosphere. Also, sea ice forms a habitat for animals. In this study, the focus is on the Southern Hemisphere where sea ice surrounds the Antarctic continent. For the winter months, we use thermal infrared satellite images where leads appear as warm, almost linear features compared to the cold ice cover. By using computer algorithms, the cracks are detected automatically. This is the first study that shows these features in the Southern Ocean. Leads not only exist ...
author2 Trier University
Laboratoire d'Océanographie et du Climat : Expérimentations et Approches Numériques (LOCEAN)
Muséum national d'Histoire naturelle (MNHN)-Institut de Recherche pour le Développement (IRD)-Institut national des sciences de l'Univers (INSU - CNRS)-Sorbonne Université (SU)-Centre National de la Recherche Scientifique (CNRS)-Institut Pierre-Simon-Laplace (IPSL (FR_636))
École normale supérieure - Paris (ENS-PSL)
Université Paris sciences et lettres (PSL)-Université Paris sciences et lettres (PSL)-Université de Versailles Saint-Quentin-en-Yvelines (UVSQ)-Commissariat à l'énergie atomique et aux énergies alternatives (CEA)-Institut national des sciences de l'Univers (INSU - CNRS)-École polytechnique (X)-Centre National d'Études Spatiales Toulouse (CNES)-Sorbonne Université (SU)-Centre National de la Recherche Scientifique (CNRS)-Université Paris Cité (UPCité)-École normale supérieure - Paris (ENS-PSL)
Université Paris sciences et lettres (PSL)-Université Paris sciences et lettres (PSL)-Université de Versailles Saint-Quentin-en-Yvelines (UVSQ)-Commissariat à l'énergie atomique et aux énergies alternatives (CEA)-École polytechnique (X)-Centre National d'Études Spatiales Toulouse (CNES)-Sorbonne Université (SU)-Centre National de la Recherche Scientifique (CNRS)-Université Paris Cité (UPCité)
European Project: 637770,H2020,ERC-2014-STG,WAPITI(2015)
format Article in Journal/Newspaper
author Reiser, F.
Willmes, S.
Hausmann, Ute
Heinemann, G.
author_facet Reiser, F.
Willmes, S.
Hausmann, Ute
Heinemann, G.
author_sort Reiser, F.
title Predominant Sea Ice Fracture Zones Around Antarctica and Their Relation to Bathymetric Features
title_short Predominant Sea Ice Fracture Zones Around Antarctica and Their Relation to Bathymetric Features
title_full Predominant Sea Ice Fracture Zones Around Antarctica and Their Relation to Bathymetric Features
title_fullStr Predominant Sea Ice Fracture Zones Around Antarctica and Their Relation to Bathymetric Features
title_full_unstemmed Predominant Sea Ice Fracture Zones Around Antarctica and Their Relation to Bathymetric Features
title_sort predominant sea ice fracture zones around antarctica and their relation to bathymetric features
publisher HAL CCSD
publishDate 2019
url https://hal.sorbonne-universite.fr/hal-02402416
https://hal.sorbonne-universite.fr/hal-02402416/document
https://hal.sorbonne-universite.fr/hal-02402416/file/Reiser_et_al-2019-Geophysical_Research_Letters.pdf
https://doi.org/10.1029/2019GL084624
genre Antarc*
Antarctic
Antarctica
Sea ice
Southern Ocean
genre_facet Antarc*
Antarctic
Antarctica
Sea ice
Southern Ocean
op_source ISSN: 0094-8276
EISSN: 1944-8007
Geophysical Research Letters
https://hal.sorbonne-universite.fr/hal-02402416
Geophysical Research Letters, 2019, 46 (21), pp.12117-12124. ⟨10.1029/2019GL084624⟩
op_relation info:eu-repo/semantics/altIdentifier/doi/10.1029/2019GL084624
info:eu-repo/grantAgreement//637770/EU/Water-mass transformation and Pathways In The Weddell Sea: uncovering the dynamics of a global climate chokepoint from In-situ measurements/WAPITI
hal-02402416
https://hal.sorbonne-universite.fr/hal-02402416
https://hal.sorbonne-universite.fr/hal-02402416/document
https://hal.sorbonne-universite.fr/hal-02402416/file/Reiser_et_al-2019-Geophysical_Research_Letters.pdf
doi:10.1029/2019GL084624
WOS: 000496009200001
op_rights info:eu-repo/semantics/OpenAccess
op_doi https://doi.org/10.1029/2019GL084624
container_title Geophysical Research Letters
container_volume 46
container_issue 21
container_start_page 12117
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spelling ftinsu:oai:HAL:hal-02402416v1 2024-04-28T07:57:17+00:00 Predominant Sea Ice Fracture Zones Around Antarctica and Their Relation to Bathymetric Features Reiser, F. Willmes, S. Hausmann, Ute Heinemann, G. Trier University Laboratoire d'Océanographie et du Climat : Expérimentations et Approches Numériques (LOCEAN) Muséum national d'Histoire naturelle (MNHN)-Institut de Recherche pour le Développement (IRD)-Institut national des sciences de l'Univers (INSU - CNRS)-Sorbonne Université (SU)-Centre National de la Recherche Scientifique (CNRS)-Institut Pierre-Simon-Laplace (IPSL (FR_636)) École normale supérieure - Paris (ENS-PSL) Université Paris sciences et lettres (PSL)-Université Paris sciences et lettres (PSL)-Université de Versailles Saint-Quentin-en-Yvelines (UVSQ)-Commissariat à l'énergie atomique et aux énergies alternatives (CEA)-Institut national des sciences de l'Univers (INSU - CNRS)-École polytechnique (X)-Centre National d'Études Spatiales Toulouse (CNES)-Sorbonne Université (SU)-Centre National de la Recherche Scientifique (CNRS)-Université Paris Cité (UPCité)-École normale supérieure - Paris (ENS-PSL) Université Paris sciences et lettres (PSL)-Université Paris sciences et lettres (PSL)-Université de Versailles Saint-Quentin-en-Yvelines (UVSQ)-Commissariat à l'énergie atomique et aux énergies alternatives (CEA)-École polytechnique (X)-Centre National d'Études Spatiales Toulouse (CNES)-Sorbonne Université (SU)-Centre National de la Recherche Scientifique (CNRS)-Université Paris Cité (UPCité) European Project: 637770,H2020,ERC-2014-STG,WAPITI(2015) 2019-11-10 https://hal.sorbonne-universite.fr/hal-02402416 https://hal.sorbonne-universite.fr/hal-02402416/document https://hal.sorbonne-universite.fr/hal-02402416/file/Reiser_et_al-2019-Geophysical_Research_Letters.pdf https://doi.org/10.1029/2019GL084624 en eng HAL CCSD American Geophysical Union info:eu-repo/semantics/altIdentifier/doi/10.1029/2019GL084624 info:eu-repo/grantAgreement//637770/EU/Water-mass transformation and Pathways In The Weddell Sea: uncovering the dynamics of a global climate chokepoint from In-situ measurements/WAPITI hal-02402416 https://hal.sorbonne-universite.fr/hal-02402416 https://hal.sorbonne-universite.fr/hal-02402416/document https://hal.sorbonne-universite.fr/hal-02402416/file/Reiser_et_al-2019-Geophysical_Research_Letters.pdf doi:10.1029/2019GL084624 WOS: 000496009200001 info:eu-repo/semantics/OpenAccess ISSN: 0094-8276 EISSN: 1944-8007 Geophysical Research Letters https://hal.sorbonne-universite.fr/hal-02402416 Geophysical Research Letters, 2019, 46 (21), pp.12117-12124. ⟨10.1029/2019GL084624⟩ tides ocean currents bathymetry MODIS Antarctic sea ice leads [SDU.STU.OC]Sciences of the Universe [physics]/Earth Sciences/Oceanography info:eu-repo/semantics/article Journal articles 2019 ftinsu https://doi.org/10.1029/2019GL084624 2024-04-05T00:43:15Z International audience Sea ice is of substantial importance for the Southern Ocean, as it insulates the relatively warm ocean from the cold atmosphere. Due to mechanical stress induced by wind and ocean currents, sea ice leads occur, which are characterized by open water and thin ice causing an increase of energy and moisture fluxes between ocean and atmosphere. Furthermore, they contribute to the ice production and provide a habitat for animals. Thus, it is important to gain information about the temporal and spatial distribution of leads on a circum-Antarctic scale. So far, no operational data set exists, which provides such information. We use thermal satellite imagery from the Moderate Resolution Imaging Spectroradiometer to derive the predominant lead patterns for 2003-2018, April-September. This study provides first results for the long-term average lead frequencies in the Southern Ocean and discusses possible links to ocean currents, tides, and the bathymetry. Plain Language Summary The polar regions are strongly influenced by sea ice, which covers large areas of the ocean's surface. Interacting with the atmosphere and the ocean, sea ice is a very dynamic surface with a large temporal and spatial variability. Under the forcing of winds and ocean currents, sea ice is subject to deformation processes causing cracks (leads) in the ice. The observation of these leads is the aim of this study since they are an important feature. For instance, open water can be found in these cracks, which enables the warm ocean (−1.7 • C) to lose energy to the cold atmosphere. Also, sea ice forms a habitat for animals. In this study, the focus is on the Southern Hemisphere where sea ice surrounds the Antarctic continent. For the winter months, we use thermal infrared satellite images where leads appear as warm, almost linear features compared to the cold ice cover. By using computer algorithms, the cracks are detected automatically. This is the first study that shows these features in the Southern Ocean. Leads not only exist ... Article in Journal/Newspaper Antarc* Antarctic Antarctica Sea ice Southern Ocean Institut national des sciences de l'Univers: HAL-INSU Geophysical Research Letters 46 21 12117 12124