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Assessment of swan and wavewatch-iii models regarding the directional wave spectra estimates based on eastern black sea measurements

dc.contributor.authorRybalko, Aleksandra
dc.contributor.authorMyslenkov, Stanislav
dc.contributor.buuauthorAkpınar, Adem
dc.contributor.buuauthorAKPINAR, ADEM
dc.contributor.buuauthorAmarouche, Khalid
dc.contributor.departmentBursa Uludağ Üniversitesi/Mühendislik Fakültesi/İnşaat Mühendisliği Bölümü.
dc.contributor.orcid0000-0001-7983-4611
dc.contributor.orcid0000-0002-9042-6851
dc.contributor.researcheridAFR-7886-2022
dc.contributor.researcheridAAC-6763-2019
dc.date.accessioned2024-10-23T05:44:30Z
dc.date.available2024-10-23T05:44:30Z
dc.date.issued2023-02-16
dc.description.abstractThe spectral wave models are often calibrated or validated based on bulk wave data derived from spectral in-formation such as the significant wave height (Hs) and mean period (Tm). However, the precision in the hind-casted spectral data was not evaluated in many seas, such as the Black Sea, due to the lack of spectral wave measurements. As part of this study, a spectral wave measuring buoy was installed near the cape Small Utrish to collect the spectral measurement data. The study objective is to assess the SWAN and WAVEWATCH-III (WWIII) models regarding the directional wave spectra estimates based on measurements conducted in the eastern Black Sea. For this purpose, the estimated spectral density distribution and spectral mean direction in terms of spectral frequency bins are assessed for both SWAN and WWIII outputs. The biases in variance densities are firstly calculated for both models at each frequency based on 14 710 spectral measurements, as well as the biases in the annual and seasonal averages. In addition, the correlation coefficients and root mean squared errors at each frequency are calculated and discussed. The accuracies in the mean direction at each spectral shape over the whole measurement period are secondly evaluated. Thirdly, the annual and seasonal averaged two-dimensional wave spectrums are discussed compared to measurements. The performances of both models are lastly verified based on bulk data measured at 8 locations on different coasts of the Black Sea. The results show that SWAN output fits better the average variance density shape at all frequency ranges f > 0.08Hz. However, it slightly overestimates the variance density in the 0.13-0.17 Hz range. In contrast to the SWAN model, WWIII data show only better correspondence in the 0.13-0.17 Hz frequency range but underestimate the lower frequency energies and overestimate higher frequency ranges. The SWAN model is therefore recommended for the spectral density estimate at seasonal and annual scales.
dc.identifier.doi10.1016/j.oceaneng.2023.113944
dc.identifier.issn0029-8018
dc.identifier.urihttps://doi.org/10.1016/j.oceaneng.2023.113944
dc.identifier.urihttps://hdl.handle.net/11452/46882
dc.identifier.volume272
dc.identifier.wos000991404500001
dc.indexed.wosWOS.SCI
dc.language.isoen
dc.publisherPergamon-elsevier Science Ltd
dc.relation.journalOcean Engineering
dc.relation.publicationcategoryMakale - Uluslararası Hakemli Dergi
dc.rightsinfo:eu-repo/semantics/closedAccess
dc.subjectMesh generation
dc.subjectCoastal regions
dc.subjectWind-sea
dc.subjectDissipation
dc.subjectVariability
dc.subjectClimate
dc.subjectBuoy
dc.subjectDirectional wave spectra
dc.subjectSpectral wave estimates
dc.subjectSwan
dc.subjectWavewatch iii
dc.subjectBlack sea
dc.subjectWave modelling
dc.subjectScience & technology
dc.subjectTechnology
dc.subjectPhysical sciences
dc.subjectEngineering, marine
dc.subjectEngineering, civil
dc.subjectEngineering, ocean
dc.subjectOceanography
dc.subjectEngineering
dc.titleAssessment of swan and wavewatch-iii models regarding the directional wave spectra estimates based on eastern black sea measurements
dc.typeArticle
dspace.entity.typePublication
relation.isAuthorOfPublication7613a1fe-c70a-4b3c-9424-e4d5cabe5d81
relation.isAuthorOfPublication.latestForDiscovery7613a1fe-c70a-4b3c-9424-e4d5cabe5d81

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