Imprints of wave climate and mean sea level variations in the dynamics of a coastal spit over the last 250 years: Cap Ferret, SW France

• Published in: Earth Surface Processes and Landforms
• Main Authors: Nahon, Alphonse, Idier, Déborah, Sénéchal, Nadia, Féniès, Hugues, Mallet, Cyril, Mugica, Julie
• Other Authors: Conseil Régional Aquitaine
• Format: Article in Journal/Newspaper
• Language: English
• Published: Wiley 2019
• Subjects: The Spit; North Atlantic; North Atlantic oscillation
• Online Access: http://dx.doi.org/10.1002/esp.4634; https://onlinelibrary.wiley.com/doi/pdf/10.1002/esp.4634; https://onlinelibrary.wiley.com/doi/full-xml/10.1002/esp.4634

Abstract In coastal areas, sea level rise (SLR) and changing wave climates are expected to be the main oceanic drivers of shoreline adjustments. These drivers have been shown to vary on a wide spectrum of spatial and temporal scales. Nonetheless, a general rule about how this variability impacts global shorelines remains to be articulated. Here, we discuss the impacts of wave climate changes and SLR on the evolution of a barrier spit–inlet system over the last 250 years. The distal end of the Cap Ferret barrier spit, SW France, has undergone large‐scale oscillations that were well correlated with variations of the decadal average of the winter North Atlantic Oscillation (NAO) index. The local wave climate hindcast supports that increased alongshore wave energy fluxes associated with the positive phase of the NAO were responsible for the updrift retreat of the spit. By opposition, the spit has elongated downdrift when waves were less energetic and more shore normal, as during the negative phase of the NAO. In addition, lower rates of SLR appeared to be necessary for the spit to develop, as higher rates of SLR very likely forced the adjacent inlet to enlarge, at the expense of the spit. These results should help to predict and detect coastal adjustments driven by climate change and by climate variability. © 2019 John Wiley & Sons, Ltd.