Extratropical transition of hurricanes in the North Atlantic and impact on the predictability of extreme events in the Mediterranean

The extratropical transition is the transformation of a tropical cyclone into an extratropical cyclone during its migration towards the midlatitudes. During its interaction with its new baroclinic environment, the cyclone can reintensify through complex dynamical and diabatic processes. It can also...

Full description

Bibliographic Details
Main Author: Pantillon, Florian
Other Authors: Laboratoire d'aérologie (LAERO), Université Toulouse III - Paul Sabatier (UT3), Université Fédérale Toulouse Midi-Pyrénées-Université Fédérale Toulouse Midi-Pyrénées-Observatoire Midi-Pyrénées (OMP), Institut de Recherche pour le Développement (IRD)-Université Toulouse III - Paul Sabatier (UT3), Université Fédérale Toulouse Midi-Pyrénées-Université Fédérale Toulouse Midi-Pyrénées-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)-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, Jean-Pierre Chaboureau, Christine Lac et Patrick Mascart
Format: Doctoral or Postdoctoral Thesis
Language:French
Published: HAL CCSD 2012
Subjects:
Online Access:https://theses.hal.science/tel-00755220
https://theses.hal.science/tel-00755220/document
https://theses.hal.science/tel-00755220/file/Manuscrit_FlorianPantillon.pdf
Description
Summary:The extratropical transition is the transformation of a tropical cyclone into an extratropical cyclone during its migration towards the midlatitudes. During its interaction with its new baroclinic environment, the cyclone can reintensify through complex dynamical and diabatic processes. It can also have a impact downstream from the strenghtening of a Rossby wave train, which quickly propagates and of which the breaking is often the trigger of extreme weather events. The complexity of dynamical and diabatic processes lead then to a reduction of the downstream predictability. Hurricanes Florence and Helene over the North Atlantic contributed that way to the triggering of extreme weather events in September 2006 in the Mediterranean, respectively, an intense precipitation event and a rarer phenomenon, a Medicane (Mediterranean hurricane). Helene was distinguished from Florence by its predominant diabatic processes during the reintensification over a warmer ocean, from which it maintained tropical characteristics. Helene was an exceptional case from its three reintensifications in three days, induced by the elongation of three filaments of potential vorticity, in addition to the development of the Medicane downstream. Both extreme weather events in the Mediterranean were missed from the midrange deterministic forecast. As diabatic processes control the impact of the hurricanes on the Rossby wave trains, the uncertainty in their description was investigated. For the first time, numerical simulations were performed with the Meso-NH model over a large domain with an explicit resolution of deep convection, taking advantage of the massive parallel computing capabilities of the model. A weak sensitivity to the horizontal resolution of the model was found in the precipitation of the hurricanes, thus in their impact on the Rossby wave trains and in the extreme weather events in the Mediterranean. The track of Helene showed instead a high sensitivity to its phasing with the Rossby wave train, that was influenced by the ...