Evolution of Climatic Forcing and Potentially ...
Type de document :
Communication dans un congrès avec actes
DOI :
Titre :
Evolution of Climatic Forcing and Potentially Eroding Events on the Coast of Northern France
Auteur(s) :
Chaverot, Sylvain [Auteur]
Université du Littoral Côte d'Opale [ULCO]
Laboratoire de géomorphologie dynamique et aménagement des littoraux [GéoDAL]
Héquette, Arnaud [Auteur]
Laboratoire d’Océanologie et de Géosciences (LOG) - UMR 8187 [LOG]
Laboratoire de géomorphologie dynamique et aménagement des littoraux [GéoDAL]
Université du Littoral Côte d'Opale [ULCO]
Cohen, Olivier [Auteur]
Laboratoire d’Océanologie et de Géosciences (LOG) - UMR 8187 [LOG]
Laboratoire de géomorphologie dynamique et aménagement des littoraux [GéoDAL]
Université du Littoral Côte d'Opale [ULCO]
Université du Littoral Côte d'Opale [ULCO]
Laboratoire de géomorphologie dynamique et aménagement des littoraux [GéoDAL]
Héquette, Arnaud [Auteur]
Laboratoire d’Océanologie et de Géosciences (LOG) - UMR 8187 [LOG]
Laboratoire de géomorphologie dynamique et aménagement des littoraux [GéoDAL]
Université du Littoral Côte d'Opale [ULCO]
Cohen, Olivier [Auteur]

Laboratoire d’Océanologie et de Géosciences (LOG) - UMR 8187 [LOG]
Laboratoire de géomorphologie dynamique et aménagement des littoraux [GéoDAL]
Université du Littoral Côte d'Opale [ULCO]
Titre de la manifestation scientifique :
5th International Conference on Coastal Dynamics (CD05)
Ville :
Barcelona
Pays :
Espagne
Date de début de la manifestation scientifique :
2005-04-04
Titre de l’ouvrage :
5th International Conference on Coastal Dynamics (CD05)
Éditeur :
American Society of Civil Engineers (ASCE)
Date de publication :
2005
Discipline(s) HAL :
Planète et Univers [physics]/Sciences de la Terre/Géomorphologie
Sciences de l'Homme et Société/Géographie
Sciences de l'Homme et Société/Géographie
Résumé en anglais : [en]
Meteorological data at Dunkirk between 1956 and 2001, show two periods of higher storminess between 1956 and 1962 and between 1972 to 1977. Tide-gauge records from Dunkirk harbor show similar results, the frequency of high ...
Lire la suite >Meteorological data at Dunkirk between 1956 and 2001, show two periods of higher storminess between 1956 and 1962 and between 1972 to 1977. Tide-gauge records from Dunkirk harbor show similar results, the frequency of high magnitude storm surges (≥100 cm) being higher during the 1960's and the second half of the 1970's. The assessment of the impacts of storm surges on coastal erosion was carried out through the use of a storm erosion susceptibility index (SESI) which integrates the magnitude of the storm surge, duration of the event, and wave height. At a medium time-scale (decades), no direct relationship was observed between the SESI and coastline evolution because potential impacts of storm surges highly depend on the upper beach morphology at the time of the event. At a short time scale, however, the use of the SESI appears to be useful for evaluating the potential effects of storms on shorelines.Lire moins >
Lire la suite >Meteorological data at Dunkirk between 1956 and 2001, show two periods of higher storminess between 1956 and 1962 and between 1972 to 1977. Tide-gauge records from Dunkirk harbor show similar results, the frequency of high magnitude storm surges (≥100 cm) being higher during the 1960's and the second half of the 1970's. The assessment of the impacts of storm surges on coastal erosion was carried out through the use of a storm erosion susceptibility index (SESI) which integrates the magnitude of the storm surge, duration of the event, and wave height. At a medium time-scale (decades), no direct relationship was observed between the SESI and coastline evolution because potential impacts of storm surges highly depend on the upper beach morphology at the time of the event. At a short time scale, however, the use of the SESI appears to be useful for evaluating the potential effects of storms on shorelines.Lire moins >
Langue :
Anglais
Comité de lecture :
Oui
Audience :
Internationale
Vulgarisation :
Non
Source :