XX century windstorms typology

Extratropical cyclones (ETCs) variability is not only a subject that raises interest among the scientific community, but also extremely important in terms of social-economical impacts. Nevertheless, the study of both the extratropical cyclones variability and windstorms impacts is still scarce, part...

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Main Author: Martins Varino, Filipa Catarina
Other Authors: Centre national de recherches météorologiques (CNRM), Institut national des sciences de l'Univers (INSU - CNRS)-Observatoire Midi-Pyrénées (OMP), Institut de Recherche pour le Développement (IRD)-Université Toulouse III - Paul Sabatier (UT3), Université de Toulouse (UT)-Université de Toulouse (UT)-Institut national des sciences de l'Univers (INSU - CNRS)-Centre National d'Études Spatiales Toulouse (CNES)-Centre National de la Recherche Scientifique (CNRS)-Météo-France-Institut de Recherche pour le Développement (IRD)-Université Toulouse III - Paul Sabatier (UT3), Université de Toulouse (UT)-Université de Toulouse (UT)-Institut national des sciences de l'Univers (INSU - CNRS)-Centre National d'Études Spatiales Toulouse (CNES)-Centre National de la Recherche Scientifique (CNRS)-Météo-France-Centre National de la Recherche Scientifique (CNRS), Université Paul Sabatier - Toulouse III, Philippe Arbogast, Gwendal Rivière, Bruno Joly
Format: Doctoral or Postdoctoral Thesis
Language:English
Published: HAL CCSD 2017
Subjects:
Online Access:https://theses.hal.science/tel-02316144
https://theses.hal.science/tel-02316144/document
https://theses.hal.science/tel-02316144/file/2017TOU30389a.pdf
id ftmeteofrance:oai:HAL:tel-02316144v1
record_format openpolar
institution Open Polar
collection Météo-France: HAL
op_collection_id ftmeteofrance
language English
topic Storm track
Cyclone tracking
20th century
ERA-20C
Arctic warming
Climate change
Hazards jet stream
Reassurance
Suivi de tempêtes
20ème siècle
Réchauffement arctique
Changement climatique
Dégâts
Courant de jet
Réassurance
[SDU.STU.ME]Sciences of the Universe [physics]/Earth Sciences/Meteorology
spellingShingle Storm track
Cyclone tracking
20th century
ERA-20C
Arctic warming
Climate change
Hazards jet stream
Reassurance
Suivi de tempêtes
20ème siècle
Réchauffement arctique
Changement climatique
Dégâts
Courant de jet
Réassurance
[SDU.STU.ME]Sciences of the Universe [physics]/Earth Sciences/Meteorology
Martins Varino, Filipa Catarina
XX century windstorms typology
topic_facet Storm track
Cyclone tracking
20th century
ERA-20C
Arctic warming
Climate change
Hazards jet stream
Reassurance
Suivi de tempêtes
20ème siècle
Réchauffement arctique
Changement climatique
Dégâts
Courant de jet
Réassurance
[SDU.STU.ME]Sciences of the Universe [physics]/Earth Sciences/Meteorology
description Extratropical cyclones (ETCs) variability is not only a subject that raises interest among the scientific community, but also extremely important in terms of social-economical impacts. Nevertheless, the study of both the extratropical cyclones variability and windstorms impacts is still scarce, particularly at time-scales that cover the twentieth century. This thesis aims to study, both storms track variability and associated losses from the beginning of the 20th century until 2010. In order to do so, the work was separated in two main parts, one witch focus on ETCs climatology during the last century using reanalysis data and another focused on loss indexes calculations and risk assessment of windstorms. The first part of this PhD concerns the study of ETCs variability after applying a tracking algorithm on the long-term ECMWF reanalysis ERA-20C. The number of ETCs per year shows three distinct periods for the moderate and deep cyclones. Two periods, one at the beginning and another at end of the century (1900-1935 and 1980-2010) for which no significant e trends are observed and a middle-century period between 1935-1980 which presents a significant positive trend. This last trend, however, a deeper analysis on this period should be done due to time-inhomogeneity of long-term reanalysis datasets. For this reason, a set of physical parameters are analysed and a physical interpretation made for each one of the periods. During the middle period, a general cooling of the atmosphere is observed, particularly at high-latitudes, which increases the meridional gradients of temperature and consequently baroclinicity and baroclinic conversion. Besides that, this increase is also observed more specifically in the Pacific (Atlantic) in the first (second) half of this period and linked with a Pacific Decadal Oscillation (Atlantic Multidecadal Oscillation) change in signs. On the opposite, the first and third periods are related with warmer polar temperatures that are more intense in the third period but never reach the ...
author2 Centre national de recherches météorologiques (CNRM)
Institut national des sciences de l'Univers (INSU - CNRS)-Observatoire Midi-Pyrénées (OMP)
Institut de Recherche pour le Développement (IRD)-Université Toulouse III - Paul Sabatier (UT3)
Université de Toulouse (UT)-Université de Toulouse (UT)-Institut national des sciences de l'Univers (INSU - CNRS)-Centre National d'Études Spatiales Toulouse (CNES)-Centre National de la Recherche Scientifique (CNRS)-Météo-France-Institut de Recherche pour le Développement (IRD)-Université Toulouse III - Paul Sabatier (UT3)
Université de Toulouse (UT)-Université de Toulouse (UT)-Institut national des sciences de l'Univers (INSU - CNRS)-Centre National d'Études Spatiales Toulouse (CNES)-Centre National de la Recherche Scientifique (CNRS)-Météo-France-Centre National de la Recherche Scientifique (CNRS)
Université Paul Sabatier - Toulouse III
Philippe Arbogast
Gwendal Rivière
Bruno Joly
format Doctoral or Postdoctoral Thesis
author Martins Varino, Filipa Catarina
author_facet Martins Varino, Filipa Catarina
author_sort Martins Varino, Filipa Catarina
title XX century windstorms typology
title_short XX century windstorms typology
title_full XX century windstorms typology
title_fullStr XX century windstorms typology
title_full_unstemmed XX century windstorms typology
title_sort xx century windstorms typology
publisher HAL CCSD
publishDate 2017
url https://theses.hal.science/tel-02316144
https://theses.hal.science/tel-02316144/document
https://theses.hal.science/tel-02316144/file/2017TOU30389a.pdf
genre Arctique*
Climate change
genre_facet Arctique*
Climate change
op_source https://theses.hal.science/tel-02316144
Meteorology. Université Paul Sabatier - Toulouse III, 2017. English. ⟨NNT : 2017TOU30389⟩
op_relation NNT: 2017TOU30389
tel-02316144
https://theses.hal.science/tel-02316144
https://theses.hal.science/tel-02316144/document
https://theses.hal.science/tel-02316144/file/2017TOU30389a.pdf
op_rights info:eu-repo/semantics/OpenAccess
_version_ 1810430882500050944
spelling ftmeteofrance:oai:HAL:tel-02316144v1 2024-09-15T17:54:34+00:00 XX century windstorms typology Typologie des tempêtes du XXe siècle Martins Varino, Filipa Catarina Centre national de recherches météorologiques (CNRM) Institut national des sciences de l'Univers (INSU - CNRS)-Observatoire Midi-Pyrénées (OMP) Institut de Recherche pour le Développement (IRD)-Université Toulouse III - Paul Sabatier (UT3) Université de Toulouse (UT)-Université de Toulouse (UT)-Institut national des sciences de l'Univers (INSU - CNRS)-Centre National d'Études Spatiales Toulouse (CNES)-Centre National de la Recherche Scientifique (CNRS)-Météo-France-Institut de Recherche pour le Développement (IRD)-Université Toulouse III - Paul Sabatier (UT3) Université de Toulouse (UT)-Université de Toulouse (UT)-Institut national des sciences de l'Univers (INSU - CNRS)-Centre National d'Études Spatiales Toulouse (CNES)-Centre National de la Recherche Scientifique (CNRS)-Météo-France-Centre National de la Recherche Scientifique (CNRS) Université Paul Sabatier - Toulouse III Philippe Arbogast Gwendal Rivière Bruno Joly 2017-09-22 https://theses.hal.science/tel-02316144 https://theses.hal.science/tel-02316144/document https://theses.hal.science/tel-02316144/file/2017TOU30389a.pdf en eng HAL CCSD NNT: 2017TOU30389 tel-02316144 https://theses.hal.science/tel-02316144 https://theses.hal.science/tel-02316144/document https://theses.hal.science/tel-02316144/file/2017TOU30389a.pdf info:eu-repo/semantics/OpenAccess https://theses.hal.science/tel-02316144 Meteorology. Université Paul Sabatier - Toulouse III, 2017. English. ⟨NNT : 2017TOU30389⟩ Storm track Cyclone tracking 20th century ERA-20C Arctic warming Climate change Hazards jet stream Reassurance Suivi de tempêtes 20ème siècle Réchauffement arctique Changement climatique Dégâts Courant de jet Réassurance [SDU.STU.ME]Sciences of the Universe [physics]/Earth Sciences/Meteorology info:eu-repo/semantics/doctoralThesis Theses 2017 ftmeteofrance 2024-06-25T00:18:08Z Extratropical cyclones (ETCs) variability is not only a subject that raises interest among the scientific community, but also extremely important in terms of social-economical impacts. Nevertheless, the study of both the extratropical cyclones variability and windstorms impacts is still scarce, particularly at time-scales that cover the twentieth century. This thesis aims to study, both storms track variability and associated losses from the beginning of the 20th century until 2010. In order to do so, the work was separated in two main parts, one witch focus on ETCs climatology during the last century using reanalysis data and another focused on loss indexes calculations and risk assessment of windstorms. The first part of this PhD concerns the study of ETCs variability after applying a tracking algorithm on the long-term ECMWF reanalysis ERA-20C. The number of ETCs per year shows three distinct periods for the moderate and deep cyclones. Two periods, one at the beginning and another at end of the century (1900-1935 and 1980-2010) for which no significant e trends are observed and a middle-century period between 1935-1980 which presents a significant positive trend. This last trend, however, a deeper analysis on this period should be done due to time-inhomogeneity of long-term reanalysis datasets. For this reason, a set of physical parameters are analysed and a physical interpretation made for each one of the periods. During the middle period, a general cooling of the atmosphere is observed, particularly at high-latitudes, which increases the meridional gradients of temperature and consequently baroclinicity and baroclinic conversion. Besides that, this increase is also observed more specifically in the Pacific (Atlantic) in the first (second) half of this period and linked with a Pacific Decadal Oscillation (Atlantic Multidecadal Oscillation) change in signs. On the opposite, the first and third periods are related with warmer polar temperatures that are more intense in the third period but never reach the ... Doctoral or Postdoctoral Thesis Arctique* Climate change Météo-France: HAL