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Tytuł artykułu

Waves, currents and seabed level change in the Port of Gdynia during extreme events

Treść / Zawartość
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Warianty tytułu
Języki publikacji
EN
Abstrakty
EN
The primary purpose of the paper is to identify port areas most exposed to extreme hydrodynamic conditions (waves, sea currents, seabed level change). The results of modelling using SWAN wave model, MIKE 3D model, and reanalysis and measurement data were used in paper. Swell may exceed 0.8 m for winds exceeding 15 m s-1 from the west and south. During extreme conditions, sea currents can reach 0.4 ms-1 in the outer part of the bay adjacent to the port. Port basins do not show changes in the thickness of the seabed for the given maximum values of bottom currents. The most extensive deposition of the seabed and shore sediments (up to 0.04 m) is found on the Gdynia-Oksywie beach adjacent to the port and the approach fairway at the offshore currents. The outer area of the main breakwater is the most exposed to erosive activity (-0.012 m).
Twórcy
autor
  • Institute of Meteorology and Water Management – National Research Institute, Gdynia, Poland
autor
  • Institute of Meteorology and Water Management – National Research Institute, Gdynia, Poland
autor
  • Institute of Meteorology and Water Management – National Research Institute, Gdynia, Poland
Bibliografia
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  • [3] Cieślikiewicz, W., Herman, A. 2001. Wind wave modelling over the Baltic Sea and the Gulf of Gdańsk.Inż. Mor. Geotech 22, 4, 173‐184 (in Polish).
  • [4] Cieślikiewicz W., Herman A. 2002. Numerical modelling of waves and currents over the Baltic Sea and the Gulf of Gdańsk.
  • [5] Cieślikiewicz W., Dudkowska A., Gic‐Grusza G. 2016. Port of Gdańsk and Port of Gdyniaʹs exposure to threats resulting from storm extremes. Journal of Polish Safety and Reliability Association, Summer Safety and Reliability Seminars, 2016, vol. 7, no. 1, pp.29‐36.
  • [6] Copernicus Climate Change Service (C3S) (2017): ERA5: Fifth generation of ECMWF atmospheric reanalyses of the global climate . Copernicus Climate Change Service Climate Data Store (CDS), date of access.https://cds.climate.copernicus.eu/cdsapp#!/home.
  • [7] Cupial A., Cieslikiewicz W. 2020. Characteristics of extreme wind wave events in the Gulf of Gdańsk and associated atmospheric conditions over the Baltic Sea. Conference Paper, EGU 2020.
  • [8] Dudkowska A., Gic‐Grusza G. 2017. Wave‐induced bedload transport – a study of the southern Baltic Sea coastal zone. Geologos 23,1. doi: 10.1515/logos‐2017‐0001.
  • [9] Gic‐Grusza, G. & Dudkowska, A., 2014. Modeling of wind wave induced sediment transport in the coastal zone of Polish marine areas (Southern Baltic). Baltic nternational Symposium (BALTIC), 2014 IEEE/OES, Tallin, 1–5.
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  • [14] Różyński G. 2010. Wave Climate in the Gulf of Gdańsk vs. Open Baltic Sea near Lubiatowo,Poland. Archives of Hydro‐Engineering and Environmental Mechanics 57, 2, 167‐176.
  • [15] Soomere T., Behrens A., Tuomi L. et al. 2008.Wave conditions in the Baltic Proper and in the Gulf of Finland during windstorm Gudrun. Natural Hazards and Earth System Science, Copernicus Publications on behalf of the European Geosciences Union. 8, 1, 37‐46.
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Uwagi
Opracowanie rekordu ze środków MEiN, umowa nr SONP/SP/546092/2022 w ramach programu "Społeczna odpowiedzialność nauki" - moduł: Popularyzacja nauki i promocja sportu (2022-2023).
Typ dokumentu
Bibliografia
Identyfikator YADDA
bwmeta1.element.baztech-b5e36e0b-84f4-4e6a-8f7d-19d3a0a5002b
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