Ocean Science Journal

, Volume 53, Issue 1, pp 133–142 | Cite as

Seabed Gradient Controlling Onshore Transport Rates of Surf Sand during Beach Retreat by Sea Level Rise

  • Hee Jun Lee
  • Hi-Il Yi


A simple relationship is proposed for the onshore transport rates of surf-zone sand to evaluate the beach retreat caused by sea level rise. It suggests that the preservation potential of surf sand is proportional inversely to the seabed gradient during beach retreat. According to this relationship, the erosional remnants of surf sand would be more readily developed on a gentler shelf collectively as transgressive sand sheets. This finding may explain the previous studies regarding the Korean shelves that proposed that the Holocene transgressive sand sheets (HTSS) occur not in the steep eastern shelf but in the gentle western shelf. In line with such presence/absence of the HTSS are the results from some coastal seismic profiles obtained in the present study. The profiles indicate that sand deposits are restricted within the nearshore in the eastern coast, whereas they are persistently traceable to the offshore HTSS in the western coast. Tide is proven to have a negligible influence on the total duration of surf-zone processes. This study may be useful in predicting the consequences of the beach retreat that takes place worldwide as sea levels rise as a result of global warming.


beach retreat sea level rise seabed gradient transgressive sand sheet sediment transport wave 


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  1. Cattaneo A, Steel RJ (2003) Transgressive deposits: a review of their variability. Earth-Sci Rev 62:187–228CrossRefGoogle Scholar
  2. Chang TS, Hong SH, Chun SS, Choi J-H (2017) Age and morphodynamics of a sandy beach fronted by a macrotidal mud flat along the west coast of Korea: a lateral headland bypass model for beach-dune formation. Geo-Mar Lett 37:316–371. doi:10.1007/s00367-016-0486-yCrossRefGoogle Scholar
  3. Chough SK, Lee HJ, Yoon SH (2000) Marine geology of Korean seas. Elsevier, Amsterdam, 313 pGoogle Scholar
  4. Chough SK, Lee HJ, Chun SS, Shin YJ (2004) Depositional processes of late Quaternary sediments in the Yellow Sea: a review. Geosci J 8:211–264CrossRefGoogle Scholar
  5. Cowell PJ, Roy PS, Jones RA (1995) Simulation of large-scale coastal change using a morphological behavior model. Mar Geol 126:45–61CrossRefGoogle Scholar
  6. Cowell PJ, Stive MJF, Niedoroda AW, Swift DJP, de Vriend HJ, Buijsman MC, Nicholls RJ, Roy PS, Kaminsky GM, Cleveringa J, Reed CW, de Boer L (2003) The coastal tract (part 2): applications of aggregated modeling of lower-order coastal change. J Coastal Res 19:828–848Google Scholar
  7. Günther H, Rosenthal W, Weare TJ, Worthington BA, Hasselmann K, Ewing JA (1979) A hybrid parametrical wave prediction model. J Geophys Res 84:5727–5738CrossRefGoogle Scholar
  8. Hasselmann, K, Barnett TP, Bouws E, Carlson H, Cartwright DE, Enke K, Ewing JA, Gienapp H, Hasselmann DE, Kruseman P, Meerburg A, Müller P, Olbers DJ, Richter K, Sell W, Walden H (1973) Measurements of wind-wave growth and swell decay during the Joint North Sea Wave Project (JONSWAP). Ergänzungsheft zur Deutschen Hydrographischen Zeitschrift Reihe A 8(12), 95 pGoogle Scholar
  9. Holthuijsen LH (2007) Waves in oceanic and coastal waters. Cambridge University Press, Cambridge, 387 pCrossRefGoogle Scholar
  10. Jin JH, Chough SK (1998) Partitioning of transgressive deposits in the southeastern Yellow Sea: a sequence stratigraphic interpretation. Mar Geol 149:79–92CrossRefGoogle Scholar
  11. Komar PD (1998) Beach processes and sedimentation. Prentice Hall, New Jersey, 544 pGoogle Scholar
  12. Larson M, Kraus NC (1995) Prediction of cross-shore sediment transport at different spatial and temporal scales. Mar Geol 126:111–127CrossRefGoogle Scholar
  13. Leatherman SP (1983) Barrier dynamics and landward migration with Holocene sea-level rise. Nature 301:415–417CrossRefGoogle Scholar
  14. Lee HJ, Chough SK (1989) Sediment distribution, dispersal and budget in the Yellow Sea. Mar Geol 87:195–205CrossRefGoogle Scholar
  15. Lee HJ, Yoo J (2012) Macrotidal beach processes dominated by winter monsoon: Byunsan, west coast of Korea. J Coastal Res 28:1177–1185CrossRefGoogle Scholar
  16. Lee HJ, Yoon SH (1997) Development of stratigraphy and sediment distribution in the northeastern Yellow Sea during Holocene sea-level rise. J Sediment Res 67:341–349Google Scholar
  17. Lee HJ, Chough SK, Jeong KS, Han SJ (1987) Geotechnical properties of sediment cores from the southeastern Yellow Sea: effects of depositional processes. Mar Geotechnol 7:37–52CrossRefGoogle Scholar
  18. Lee SH, Lee HJ, Park J-Y, Jeong EY, Yoo J, Ha HK, Shin CW, Park C (2013) Possible origin of coastal sands and their longterm distribution along the high slope-gradient, wave-dominated eastern coast, Korea. Geosci J 17:163–172CrossRefGoogle Scholar
  19. MOF (1997) Long-term (1979–1996) simulation of waves around the Korean Peninsula. Ministry of Oceans and Fisheries (MOF), 361 p (in Korean)Google Scholar
  20. Penland S, Boyd R, Suter JR (1988) Transgressive depositional systems of the Mississippi delta plain: a model for barrier shoreline and shelf sand development. J Sediment Petrol 58:932–949Google Scholar
  21. Penland S, Suter JR, Boyd R (1985) Barrier island arcs along abandoned Mississippi River deltas. Mar Geol 63:197–233CrossRefGoogle Scholar
  22. Saito Y, Nishimura A, Matsumoto E (1989) Transgressive sand shelf covering the shelf and upper slope off Sendai, northeast Japan. Mar Geol 89:245–258CrossRefGoogle Scholar
  23. Sallenger AH, Holman RA (1985) Wave energy saturation on a natural beach of variable slope. J Geophys Res 90(C6):11939–11944CrossRefGoogle Scholar
  24. Soulsby R (1997) Dynamics of marine sands. Thomas Telford, London, 249 pGoogle Scholar
  25. Storms JEA, Weltje GJ, Terra GJ, Cattaneo A, Trincardi F (2008) Coastal dynamics under conditions of rapid sea-level rise: late Pleistocene to early Holocene evolution of barrier-lagoon systems on the northern Adriatic shelf (Italy). Quaternary Sci Rev 27:1107–1123CrossRefGoogle Scholar
  26. Swift DJP, Phillips S, Thorne JA (1991) Sedimentation on continental margins: V. Parasequences. In: Swift DJP, Oertel GF, Tillman RW, Thorne JA (eds) Shelf sand and sandstone bodies–geometry, facies and sequence stratigraphy. Blackwell Scientific Publications, London, pp 153–188Google Scholar
  27. Van Rijn LC (1993) Principles of sediment transport in rivers, estuaries and coastal Seas. Aqua Publications, Amsterdam, 497 pGoogle Scholar
  28. Yang BC, Dalrymple RW, Chun SS, Lee HJ (2006) Transgressive sedimentation and stratigraphic evolution of a wave-dominated macrotidal coast, western Korea. Mar Geol 235:35–48CrossRefGoogle Scholar

Copyright information

© Korea Institute of Ocean Science & Technology (KIOST) and the Korean Society of Oceanography (KSO) and Springer Science+Business Media B.V., part of Springer Nature 2017

Authors and Affiliations

  1. 1.Marine Geology and Geophysic DivisionKIOSTAnsanKorea

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