Role of Arctic sea ice decline on the mid-latitude climate : atmospheric teleconnections
The Arctic has been warming twice as fast as the whole globe since the preindustrial era: this phenomenon is known as Arctic amplification. Arctic amplification and associated Arctic sea ice decline can affect the climate locally. It has also been shown to affect the large-scale atmospheric circulat...
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Language: | French |
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Online Access: | https://theses.hal.science/tel-03611295 https://theses.hal.science/tel-03611295/document https://theses.hal.science/tel-03611295/file/2020TOU30314b.pdf |
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ftccsdartic:oai:HAL:tel-03611295v1 2023-06-11T04:03:12+02:00 Role of Arctic sea ice decline on the mid-latitude climate : atmospheric teleconnections Rôle du déclin de la glace de mer en Arctique sur le climat des moyennes latitudes : téléconnexions atmosphériques Chripko, Svenya Climat, Environnement, Couplages et Incertitudes Toulouse (CECI) Institut national des sciences de l'Univers (INSU - CNRS)-Centre Européen de Recherche et de Formation Avancée en Calcul Scientifique - CERFACS (CERFACS)-Centre National de la Recherche Scientifique (CNRS) Université Paul Sabatier - Toulouse III Rym Msadek Emilia Sanchez-Gomez 2020-11-20 https://theses.hal.science/tel-03611295 https://theses.hal.science/tel-03611295/document https://theses.hal.science/tel-03611295/file/2020TOU30314b.pdf fr fre HAL CCSD NNT: 2020TOU30314 tel-03611295 https://theses.hal.science/tel-03611295 https://theses.hal.science/tel-03611295/document https://theses.hal.science/tel-03611295/file/2020TOU30314b.pdf info:eu-repo/semantics/OpenAccess https://theses.hal.science/tel-03611295 Climatologie. Université Paul Sabatier - Toulouse III, 2020. Français. ⟨NNT : 2020TOU30314⟩ Arctic sea ice Mid-latitudes Teleconnections Atmospheric circulation Atmospheric variability Arctic oscillation Climate models Glace de mer arctique Moyennes latitudes Téléconnexions Circulation atmosphérique Variabilité atmosphérique Oscillation arctique Modèles climatiques [SDU.STU.CL]Sciences of the Universe [physics]/Earth Sciences/Climatology info:eu-repo/semantics/doctoralThesis Theses 2020 ftccsdartic 2023-05-06T23:50:29Z The Arctic has been warming twice as fast as the whole globe since the preindustrial era: this phenomenon is known as Arctic amplification. Arctic amplification and associated Arctic sea ice decline can affect the climate locally. It has also been shown to affect the large-scale atmospheric circulation beyond the Arctic, yielding changes in the mid-latitude climate. However, the mechanisms beneath this linkage are still poorly understood. The objective of this thesis is to bring more insight into these mechanisms. For that purpose, we have defined and run sensitivity experiments that allow to isolate the effect of Arctic sea ice decline from other climate forcings. In these experiments, which have been done with the CNRM-CM6 climate model using different horizontal resolutions, sea ice albedo is reduced to the ocean value, leading to an increase in absorbed solar radiation and a reduction of sea ice especially in summer. We first evaluate the model mean state and its representation of Arctic-to-mid-latitude linkages. This analysis suggests that increasing the horizontal resolution in the atmosphere and ocean generally leads to more realistic mean climate conditions in the Northern Hemisphere. We further show that linkages between atmospheric and sea ice variability are consistent between the model and the observations. These results indicate that Arctic sea ice influence on the atmosphere is hardly detectable in observations and in free-running models because of the large internal variability, which stresses the need to properly isolate this link using dedicated sensitivity experiments. Secondly, we focus on the rapid atmospheric response during autumn and winter, when Arctic amplification is maximum. Using a dynamical adjustment method based on a regional reconstruction of circulation analogs, the mechanisms of the regional temperature response are investigated. We show that the sea-ice-induced warming over North America and Europe can be explained by : (i) cyclonic changes in circulation that favor warm air ... Doctoral or Postdoctoral Thesis albedo Arctic Arctique* Sea ice Archive ouverte HAL (Hyper Article en Ligne, CCSD - Centre pour la Communication Scientifique Directe) Arctic |
institution |
Open Polar |
collection |
Archive ouverte HAL (Hyper Article en Ligne, CCSD - Centre pour la Communication Scientifique Directe) |
op_collection_id |
ftccsdartic |
language |
French |
topic |
Arctic sea ice Mid-latitudes Teleconnections Atmospheric circulation Atmospheric variability Arctic oscillation Climate models Glace de mer arctique Moyennes latitudes Téléconnexions Circulation atmosphérique Variabilité atmosphérique Oscillation arctique Modèles climatiques [SDU.STU.CL]Sciences of the Universe [physics]/Earth Sciences/Climatology |
spellingShingle |
Arctic sea ice Mid-latitudes Teleconnections Atmospheric circulation Atmospheric variability Arctic oscillation Climate models Glace de mer arctique Moyennes latitudes Téléconnexions Circulation atmosphérique Variabilité atmosphérique Oscillation arctique Modèles climatiques [SDU.STU.CL]Sciences of the Universe [physics]/Earth Sciences/Climatology Chripko, Svenya Role of Arctic sea ice decline on the mid-latitude climate : atmospheric teleconnections |
topic_facet |
Arctic sea ice Mid-latitudes Teleconnections Atmospheric circulation Atmospheric variability Arctic oscillation Climate models Glace de mer arctique Moyennes latitudes Téléconnexions Circulation atmosphérique Variabilité atmosphérique Oscillation arctique Modèles climatiques [SDU.STU.CL]Sciences of the Universe [physics]/Earth Sciences/Climatology |
description |
The Arctic has been warming twice as fast as the whole globe since the preindustrial era: this phenomenon is known as Arctic amplification. Arctic amplification and associated Arctic sea ice decline can affect the climate locally. It has also been shown to affect the large-scale atmospheric circulation beyond the Arctic, yielding changes in the mid-latitude climate. However, the mechanisms beneath this linkage are still poorly understood. The objective of this thesis is to bring more insight into these mechanisms. For that purpose, we have defined and run sensitivity experiments that allow to isolate the effect of Arctic sea ice decline from other climate forcings. In these experiments, which have been done with the CNRM-CM6 climate model using different horizontal resolutions, sea ice albedo is reduced to the ocean value, leading to an increase in absorbed solar radiation and a reduction of sea ice especially in summer. We first evaluate the model mean state and its representation of Arctic-to-mid-latitude linkages. This analysis suggests that increasing the horizontal resolution in the atmosphere and ocean generally leads to more realistic mean climate conditions in the Northern Hemisphere. We further show that linkages between atmospheric and sea ice variability are consistent between the model and the observations. These results indicate that Arctic sea ice influence on the atmosphere is hardly detectable in observations and in free-running models because of the large internal variability, which stresses the need to properly isolate this link using dedicated sensitivity experiments. Secondly, we focus on the rapid atmospheric response during autumn and winter, when Arctic amplification is maximum. Using a dynamical adjustment method based on a regional reconstruction of circulation analogs, the mechanisms of the regional temperature response are investigated. We show that the sea-ice-induced warming over North America and Europe can be explained by : (i) cyclonic changes in circulation that favor warm air ... |
author2 |
Climat, Environnement, Couplages et Incertitudes Toulouse (CECI) Institut national des sciences de l'Univers (INSU - CNRS)-Centre Européen de Recherche et de Formation Avancée en Calcul Scientifique - CERFACS (CERFACS)-Centre National de la Recherche Scientifique (CNRS) Université Paul Sabatier - Toulouse III Rym Msadek Emilia Sanchez-Gomez |
format |
Doctoral or Postdoctoral Thesis |
author |
Chripko, Svenya |
author_facet |
Chripko, Svenya |
author_sort |
Chripko, Svenya |
title |
Role of Arctic sea ice decline on the mid-latitude climate : atmospheric teleconnections |
title_short |
Role of Arctic sea ice decline on the mid-latitude climate : atmospheric teleconnections |
title_full |
Role of Arctic sea ice decline on the mid-latitude climate : atmospheric teleconnections |
title_fullStr |
Role of Arctic sea ice decline on the mid-latitude climate : atmospheric teleconnections |
title_full_unstemmed |
Role of Arctic sea ice decline on the mid-latitude climate : atmospheric teleconnections |
title_sort |
role of arctic sea ice decline on the mid-latitude climate : atmospheric teleconnections |
publisher |
HAL CCSD |
publishDate |
2020 |
url |
https://theses.hal.science/tel-03611295 https://theses.hal.science/tel-03611295/document https://theses.hal.science/tel-03611295/file/2020TOU30314b.pdf |
geographic |
Arctic |
geographic_facet |
Arctic |
genre |
albedo Arctic Arctique* Sea ice |
genre_facet |
albedo Arctic Arctique* Sea ice |
op_source |
https://theses.hal.science/tel-03611295 Climatologie. Université Paul Sabatier - Toulouse III, 2020. Français. ⟨NNT : 2020TOU30314⟩ |
op_relation |
NNT: 2020TOU30314 tel-03611295 https://theses.hal.science/tel-03611295 https://theses.hal.science/tel-03611295/document https://theses.hal.science/tel-03611295/file/2020TOU30314b.pdf |
op_rights |
info:eu-repo/semantics/OpenAccess |
_version_ |
1768377708464570368 |