Extreme Wave Analysis by Integrating Model and Wave Buoy Data

Estimating the extreme values of significant wave height (HS), generally described by the HS return period TR function HS(TR) and by its confidence intervals, is a necessity in many branches of coastal science and engineering. The availability of indirect wave data generated by global and regional w...

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Published in:Water
Main Authors: Dentale F., Furcolo P., Carratelli E. P., Reale F., Contestabile P., Tomasicchio G.
Other Authors: Dentale, F., Furcolo, P., Carratelli, E. P., Reale, F., Contestabile, P., Tomasicchio, G.
Format: Article in Journal/Newspaper
Language:English
Published: 2018
Subjects:
Online Access:http://hdl.handle.net/11587/435221
https://doi.org/10.3390/w10040373
http://www.mdpi.com/2073-4441/10/4/373/pdf
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spelling ftunivsalento:oai:iris.unisalento.it:11587/435221 2024-04-14T08:15:53+00:00 Extreme Wave Analysis by Integrating Model and Wave Buoy Data Dentale F. Furcolo P. Carratelli E. P. Reale F. Contestabile P. Tomasicchio G. Dentale, F. Furcolo, P. Carratelli, E. P. Reale, F. Contestabile, P. Tomasicchio, G. 2018 ELETTRONICO http://hdl.handle.net/11587/435221 https://doi.org/10.3390/w10040373 http://www.mdpi.com/2073-4441/10/4/373/pdf eng eng info:eu-repo/semantics/altIdentifier/wos/WOS:000434954900027 volume:10 firstpage:373 lastpage:387 numberofpages:15 journal:WATER http://hdl.handle.net/11587/435221 doi:10.3390/w10040373 info:eu-repo/semantics/altIdentifier/scopus/2-s2.0-85044362596 http://www.mdpi.com/2073-4441/10/4/373/pdf Gulf of Mexico Mediterranean Sea North Atlantic Spanish coast Small scale storm variation Wave extreme event Wave modeling info:eu-repo/semantics/article 2018 ftunivsalento https://doi.org/10.3390/w10040373 2024-03-21T18:06:30Z Estimating the extreme values of significant wave height (HS), generally described by the HS return period TR function HS(TR) and by its confidence intervals, is a necessity in many branches of coastal science and engineering. The availability of indirect wave data generated by global and regional wind and wave model chains have brought radical changes to the estimation procedures of such probability distribution-weather and wave modeling systems are routinely run all over the world, and HS time series for each grid point are produced and published after assimilation (analysis) of the ground truth. However, while the sources of such indirect data are numerous, and generally of good quality, many aspects of their procedures are hidden to the users, who cannot evaluate the reliability and the limits of the HS(TR) deriving from such data. In order to provide a simple engineering tool to evaluate the probability of extreme sea-states as well as the quality of such estimates, we propose here a procedure based on integrating HS time series generated by model chains with those recorded by wave buoys in the same area. Article in Journal/Newspaper North Atlantic Università del Salento: CINECA IRIS Water 10 4 373
institution Open Polar
collection Università del Salento: CINECA IRIS
op_collection_id ftunivsalento
language English
topic Gulf of Mexico
Mediterranean Sea
North Atlantic Spanish coast
Small scale storm variation
Wave extreme event
Wave modeling
spellingShingle Gulf of Mexico
Mediterranean Sea
North Atlantic Spanish coast
Small scale storm variation
Wave extreme event
Wave modeling
Dentale F.
Furcolo P.
Carratelli E. P.
Reale F.
Contestabile P.
Tomasicchio G.
Extreme Wave Analysis by Integrating Model and Wave Buoy Data
topic_facet Gulf of Mexico
Mediterranean Sea
North Atlantic Spanish coast
Small scale storm variation
Wave extreme event
Wave modeling
description Estimating the extreme values of significant wave height (HS), generally described by the HS return period TR function HS(TR) and by its confidence intervals, is a necessity in many branches of coastal science and engineering. The availability of indirect wave data generated by global and regional wind and wave model chains have brought radical changes to the estimation procedures of such probability distribution-weather and wave modeling systems are routinely run all over the world, and HS time series for each grid point are produced and published after assimilation (analysis) of the ground truth. However, while the sources of such indirect data are numerous, and generally of good quality, many aspects of their procedures are hidden to the users, who cannot evaluate the reliability and the limits of the HS(TR) deriving from such data. In order to provide a simple engineering tool to evaluate the probability of extreme sea-states as well as the quality of such estimates, we propose here a procedure based on integrating HS time series generated by model chains with those recorded by wave buoys in the same area.
author2 Dentale, F.
Furcolo, P.
Carratelli, E. P.
Reale, F.
Contestabile, P.
Tomasicchio, G.
format Article in Journal/Newspaper
author Dentale F.
Furcolo P.
Carratelli E. P.
Reale F.
Contestabile P.
Tomasicchio G.
author_facet Dentale F.
Furcolo P.
Carratelli E. P.
Reale F.
Contestabile P.
Tomasicchio G.
author_sort Dentale F.
title Extreme Wave Analysis by Integrating Model and Wave Buoy Data
title_short Extreme Wave Analysis by Integrating Model and Wave Buoy Data
title_full Extreme Wave Analysis by Integrating Model and Wave Buoy Data
title_fullStr Extreme Wave Analysis by Integrating Model and Wave Buoy Data
title_full_unstemmed Extreme Wave Analysis by Integrating Model and Wave Buoy Data
title_sort extreme wave analysis by integrating model and wave buoy data
publishDate 2018
url http://hdl.handle.net/11587/435221
https://doi.org/10.3390/w10040373
http://www.mdpi.com/2073-4441/10/4/373/pdf
genre North Atlantic
genre_facet North Atlantic
op_relation info:eu-repo/semantics/altIdentifier/wos/WOS:000434954900027
volume:10
firstpage:373
lastpage:387
numberofpages:15
journal:WATER
http://hdl.handle.net/11587/435221
doi:10.3390/w10040373
info:eu-repo/semantics/altIdentifier/scopus/2-s2.0-85044362596
http://www.mdpi.com/2073-4441/10/4/373/pdf
op_doi https://doi.org/10.3390/w10040373
container_title Water
container_volume 10
container_issue 4
container_start_page 373
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