Wave energy asymmetry in shallow bays

Storm surges along the coastline of the United States are often driven by along‐shore winds triggering cross‐shore Ekman transport. Here we show that this mechanism creates ideal conditions for large wave events in the shallow bays characterizing much of the Atlantic and Gulf of Mexico coastlines. A...

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Veröffentlicht in:Geophysical research letters 2010-12, Vol.37 (24), p.np-n/a
Hauptverfasser: Fagherazzi, S., Mariotti, G., Porter, J. H., McGlathery, K. J., Wiberg, P. L.
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container_issue 24
container_start_page np
container_title Geophysical research letters
container_volume 37
creator Fagherazzi, S.
Mariotti, G.
Porter, J. H.
McGlathery, K. J.
Wiberg, P. L.
description Storm surges along the coastline of the United States are often driven by along‐shore winds triggering cross‐shore Ekman transport. Here we show that this mechanism creates ideal conditions for large wave events in the shallow bays characterizing much of the Atlantic and Gulf of Mexico coastlines. A positive feedback enhances wave formation during along‐shore wind events, affecting the spatial distribution of waves and wave‐forced erosion in shallow bays at a continental scale.
doi_str_mv 10.1029/2010GL045254
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source Wiley Journals; Wiley Online Library Free Content; Wiley-Blackwell AGU Digital Library; EZB-FREE-00999 freely available EZB journals
subjects Asymmetry
Bays
Coastlines
Earth sciences
Earth, ocean, space
Ekman transport
Erosion
Exact sciences and technology
Geophysics
Gulf of Mexico
Marine geology
Physical oceanography
Spatial distribution
storm surge
Storm surges
Transport
Wave energy
wind waves
title Wave energy asymmetry in shallow bays
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