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The ability of a barotropic model to simulate sea level extremes of meteorological origin in the Mediterranean Sea, including those caused by explosive cyclones

The ability of a barotropic model to simulate sea level extremes of meteorological origin in the Mediterranean Sea, including those caused by explosive cyclones
The ability of a barotropic model to simulate sea level extremes of meteorological origin in the Mediterranean Sea, including those caused by explosive cyclones
Storm surges are responsible for great damage to coastal property and loss of life every year. Coastal management and adaptation practices are essential to reduce such damage. Numerical models provide a useful tool for informing these practices as they simulate sea level with high spatial resolution. Here we investigate the ability of a barotropic version of the HAMSOM model to simulate sea level extremes of meteorological origin in the Mediterranean Sea, including those caused by explosive cyclones. For this purpose, the output of the model is compared to hourly sea level observations from six tide gauge records (Valencia, Barcelona, Marseille, Civitavecchia, Trieste, and Antalya). It is found that the model underestimates the positive extremes significantly at all stations, in some cases by up to 65%. At Trieste, the model can also sometimes overestimate the extremes significantly. The differences between the model and the residuals are not constant for extremes of a given height, which limits the applicability of the numerical model for storm surge forecasting because calibration is difficult. The 50 and 10 year return levels are reasonably well captured by the model at all stations except Barcelona and Marseille, where they are underestimated by over 30%. The number of exceedances of the 99.9th and 99.95% percentiles over a period of 25 years is severely underestimated by the model at all stations. The skill of the model for predicting the timing and value of the storm surges seems to be higher for the events associated with explosive cyclones at all stations.
sea level extremes, numerical model, explosive cyclones, storm surge
2169-9275
7840-7853
Calafat, F.M.
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Avgoustoglou, E.
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Jordà, G.
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Flocas, H.
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Zodiatis, G.
ad317639-8f2e-47ca-909c-b21217ce2629
Tsimplis, M.N.
df6dd749-cda4-46ec-983c-bf022d737031
Kouroutzoglou, J.
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Calafat, F.M.
7c43d62a-c376-446c-93b4-87d4c1bd9d05
Avgoustoglou, E.
dcfbd84a-ea57-4a8a-9c52-e43f994df763
Jordà, G.
b115333d-2852-49d8-bfc2-f42827580201
Flocas, H.
885f9992-e7a8-4cb8-a77b-c7941a699560
Zodiatis, G.
ad317639-8f2e-47ca-909c-b21217ce2629
Tsimplis, M.N.
df6dd749-cda4-46ec-983c-bf022d737031
Kouroutzoglou, J.
c9bb60d4-f4b6-4ab4-a228-36b72e6827be

Calafat, F.M., Avgoustoglou, E., Jordà, G., Flocas, H., Zodiatis, G., Tsimplis, M.N. and Kouroutzoglou, J. (2014) The ability of a barotropic model to simulate sea level extremes of meteorological origin in the Mediterranean Sea, including those caused by explosive cyclones. Journal of Geophysical Research: Oceans, 119 (11), 7840-7853. (doi:10.1002/2014JC010360).

Record type: Article

Abstract

Storm surges are responsible for great damage to coastal property and loss of life every year. Coastal management and adaptation practices are essential to reduce such damage. Numerical models provide a useful tool for informing these practices as they simulate sea level with high spatial resolution. Here we investigate the ability of a barotropic version of the HAMSOM model to simulate sea level extremes of meteorological origin in the Mediterranean Sea, including those caused by explosive cyclones. For this purpose, the output of the model is compared to hourly sea level observations from six tide gauge records (Valencia, Barcelona, Marseille, Civitavecchia, Trieste, and Antalya). It is found that the model underestimates the positive extremes significantly at all stations, in some cases by up to 65%. At Trieste, the model can also sometimes overestimate the extremes significantly. The differences between the model and the residuals are not constant for extremes of a given height, which limits the applicability of the numerical model for storm surge forecasting because calibration is difficult. The 50 and 10 year return levels are reasonably well captured by the model at all stations except Barcelona and Marseille, where they are underestimated by over 30%. The number of exceedances of the 99.9th and 99.95% percentiles over a period of 25 years is severely underestimated by the model at all stations. The skill of the model for predicting the timing and value of the storm surges seems to be higher for the events associated with explosive cyclones at all stations.

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Accepted/In Press date: 21 November 2014
e-pub ahead of print date: 21 November 2014
Published date: November 2014
Keywords: sea level extremes, numerical model, explosive cyclones, storm surge
Organisations: Marine Physics and Ocean Climate

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Local EPrints ID: 372059
URI: http://eprints.soton.ac.uk/id/eprint/372059
ISSN: 2169-9275
PURE UUID: 5290f0dd-6aea-4a1d-9558-5206a7bf74b2

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Date deposited: 24 Nov 2014 10:53
Last modified: 14 Mar 2024 18:30

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Contributors

Author: F.M. Calafat
Author: E. Avgoustoglou
Author: G. Jordà
Author: H. Flocas
Author: G. Zodiatis
Author: M.N. Tsimplis
Author: J. Kouroutzoglou

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