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Coastal Processes at Selected Shore Segments of South Baltic Sea and Gulf of Tonkin (South China Sea)

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The paper presents a comparative analysis of physical processes occurring at two different coasts, which belong to two different geographic zones, namely a subtropical region exposed to monsoons and typhoons and a region of temperate climate with ice-snowy winter season. The former coast comprises sandy shores nearby Lubiatowo and the Hel Peninsula, located at the south Baltic Sea in Poland. The shore at Lubiatowo is relatively stable in the long run, while the shore along Hel Peninsula is mostly vulnerable to erosion and strongly protected by use of various measures (groins, seawall and artificial beach nourishment). The second site is the eroded (and partly protected by dikes) coast at Hai Hau in the Gulf of Tonkin (the South China Sea, Vietnam). This shore segment is built of mixtures of sandy and cohesive material, comprising both marine sands and river-borne sediments which nourish the coastal zone at the Red River mouth, located northwards of the Hai Hau beach. The present analysis is focused on differences and similarities of hydro- and morphodynamics between the above coastal zones in various time and spatial scales. The analysis shows that regional climatic and environmental conditions, associated with geographical zones, play a key role in dynamic evolution of the coastal regions and necessitate different engineering activities against erosion and flooding.
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autor
  • Institute of Hydro-Engineering of the Polish Academy of Sciences (IBW PAN), Kościerska 7, 80-328 Gdańsk, Poland, rafi@ibwpan.gda.pl
Bibliografia
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  • 2. Lien N. T. V, Moi N. V. and Nga N. T. K. (2005) Compilation and analysis of data collected on hydro-meteorology, bathymetry and beach change, Proc. The first scientific workshop on coastline evolution, Vietnam – Sweden research cooperation program, project: ‘The evolution and sustainable development of the coastal areas in Vietnam’, 14–28.
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  • 7. Pruszak Z., Ninh P. V., Szmytkiewicz M., Hung N. M. and Ostrowski R. (2005a) Hydrology and morphology of two river mouth regions (temperate Vistula Delta and subtropical Red River Delta), Oceanologia, 47 (3), 365–385.
  • 8. Pruszak Z., Rózynski G., Szmytkiewicz M. and Ostrowski R. (2005b) Infragravity waves and rhythmic shoreline forms at a non-tidal, sandy coast with multiple bars, Proc. of 29th ICCE, Ed. Jane McKee Smith, New Jersey, London, Singapore: World Scientific Publishing Company, 3, 2568–2580.
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  • 12. Quynh D. N., Manh D. V., Lien N. T. V. and Duyet T. T. N. (2006) Modeling of Sea Level and Nearshore Circulation in the Red River Delta Coastal Zone, Proc. of the 1stScientific Workshop on Coastal Evolution, Thinh Long, Vietnam, ed. by M. Larson and N.M. Hung, 64–74.
  • 13. Rózynski G., Larson M. and Pruszak Z. (2001) Forced and self-organized shoreline response for a beach in the southern Baltic Sea determined through singular spectrum analysis, Coastal Engineering, 43 (1), 41–58.
  • 14. Szmytkiewicz M., Biegowski J., Kaczmarek L. M., Okrój T., Ostrowski R., Pruszak Z., Rózynski G. and Skaja M. (2000) Coastline changes nearby harbour structures: comparative analysis of one-line models versus field data, Coastal Engineering, 40 (2), 119–139.
  • 15. The East Sea Monograph (2003) Volume II: Meteorology, Marine Hydrology and Marine Hydrodynamics, ed. by Ninh P. V., Publishing House of Hanoi State University, Hanoi.
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  • 17. Vinh T., Pruszak Z., Huan N. and Kant G. (1997) Sea dike erosion and coastal retreat at Nam Ha Province, Vietnam, Proc. of 25th ICCE, New York: ASCE, 4, 2820–2828.
  • 18. VVA Report – A8 (1995) Vietnam Coastal Zone Vulnerability Assessment and First Steps Towards Integrated Coastal Zone Management, Report No. 2, Hanoi/Gdansk/the Hague (Part 8 – Report on Wave Characteristics).
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Typ dokumentu
Bibliografia
Identyfikator YADDA
bwmeta1.element.baztech-article-BAT8-0014-0001
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