Storminess interannual variability and coastal hazards over the south-western Spanish coast: links to large scale atmospheric forcing

• Published in: Géomorphologie : relief, processus, environnement
• Main Authors: Plomaritis, Theocharis A., Benavente, Javier, Laiz, Irene, del Río, Laura
• Format: Article in Journal/Newspaper
• Language: English
• Published: Groupe français de géomorphologie 2014
• Subjects: NAO; EA; storms; Cadiz; ONA; tempêtes; geo; envir; Tempêtes; North Atlantic; North Atlantic oscillation
• Online Access: http://journals.openedition.org/geomorphologie/10728

In the context of increased coastal hazards through storminess variability, the danger of coastal damages and/or morphological changes is related to the sum of mean sea level conditions, storm surge and maximum wave height and run up values. In order to better understand the physical processes that cause the interannual variability of the above parameters a reanalysis record (HIPOCAS) of the last 44 years was used. The HIPOCAS time-series was validated with real wind, wave and sea-level data using linear and vector correlation methods. In the present work changes in the duration, frequency, chronology and approach direction of the Atlantic storms over the Spanish Gulf of Cadiz (SW Iberian Peninsula) were identified by computing various storm characteristics such as maximum wave height, total energy per storm and storm groupiness. The obtained time-series were compared with large-scale atmospheric indices such as the North Atlantic Oscillation (NAO) and the East Atlantic pattern (EA). The results show a good correlation between negative NAO values and increased storminess over the entire Gulf of Cadiz. Furthermore, negative NAO values were correlated with high mean sea level values and westerly and south-westerly wind events, indicating higher probability of coastal risks. The above results were compared with coastal inundation events that took place over the last winter seasons in the province of Cadiz. Dans le contexte de l’augmentation des risques côtiers, à travers la variabilité de la fréquence et de l’intensité des tempêtes, les dommages aux infrastructures côtières et les changements morphologiques des côtes sont mises en rapport avec la prise en compte conjointe du niveau moyen de la mer, des surcotes dues aux tempêtes, des valeurs maximales de hauteur de vague et des valeurs du jet de rive. Afin de mieux comprendre les processus physiques qui génèrent la variabilité interannuelle de ces paramètres, une réanalyse des enregistrements (HIPOCAS) de ces 44 dernières années a été effectuée. La série ...