North-Atlantic Oscillation and regional-scale sea-surge variability in Gulf of Lions during the 20th century

• Main Authors: Ullmann, Albin, Moron, Vincent
• Other Authors: Centre de Recherches de Climatologie (CRC), Université de Bourgogne (UB)-Centre National de la Recherche Scientifique (CNRS), International Research Institute for Climate and Society (IRI), Earth Institute at Columbia University, Columbia University New York -Columbia University New York, Centre Européen de Recherche et d'Enseignement des Géosciences de l'Environnement (CEREGE), Institut de Recherche pour le Développement (IRD)-Institut National de la Recherche Agronomique (INRA)-Aix Marseille Université (AMU)-Collège de France (CdF (institution))-Institut national des sciences de l'Univers (INSU - CNRS)-Centre National de la Recherche Scientifique (CNRS)
• Format: Article in Journal/Newspaper
• Language: English
• Published: HAL CCSD 2010
• Subjects: sea surge; wind conditions; North-Atlantic Oscillation; Mediterranean Sea; multi-decadal variations; [SDU.STU.CL]Sciences of the Universe [physics]/Earth Sciences/Climatology; [SDE.MCG]Environmental Sciences/Global Changes; Dent; La Dent; Iceland; North Atlantic; North Atlantic oscillation
• Online Access: https://hal.science/hal-00447324; https://hal.science/hal-00447324/document; https://hal.science/hal-00447324/file/Ullmann_Moron.pdf

Article soumis International audience Sea-surge variations recorded at three tide-gauge stations (Grau-de-la-Dent, Sète, and Port-Vendres) around the Gulf of Lions (Northwest Mediterranean Sea) are mostly locally forced by onshore winds blowing from 90° to 180° related to an atmospheric depression usually centered between the Bay of Biscay and the British Island, which is more prevalent during the negative phase of the North-Atlantic Oscillation (NAO). During the second half of the 20th century, the long-term increase of sea-surge height at Grau-de-la-Dent finds no counterpart in the positive deviation of the NAO. The relationship between the monthly frequency of sea surges > 20 cm at Grau-de-la-Dent and the monthly mean NAO Index significantly strengthens from 1975. This is synchronous with the eastward shift of the two main centers of the NAO (i.e. Iceland low and Azores high) and an increase of the occurrence of depressions near the Bay of Biscay and of surge-related onshore winds in the Gulf of Lions during negative phases of the NAO.