DOI QR코드

DOI QR Code

Comparisons of the Environmental Characteristics of Intertidal Beach and Mudflat

  • Kim, Tae-Rim (Department of Coastal Construction Engineering, Kunsan University)
  • Published : 2009.06.28

Abstract

The characteristics of morphological shapes, wave heights, tidal ranges and sediment sizes are observed and compared between intertidal beach and mudflat. The Mohang sand beach, southwest coast of Korea, is located just next to the large mudflat and has tidal range over 5 meters. Wave measurements are conducted at each entrance of the beach and mudflat as well as at the outside waters representing the incident waves to these different coastal environments. The morphological characteristics are also examined including the sediment size and the slope of the bathymetry, For the observation of morphological shapes, camera monitoring technique is used to measure the spatial information of intertidal bathymetry. The water lines moving on the intertidal flat/beach durinq a flood indicate depth contours between low and high water lines. The water lines extracted from the consecutive images are rectified to get the ground coordinates of each depth contours and integrated to provide three dimensional information of intertidal topography. The wave data show that sand beach is in the condition of severer wave forcing but tidal range is almost identical in both environment. The slope of the mudflat is much milder than the sand beach with finer sediment.

Keywords

References

  1. Aagaard T., A. Kroon, S. Andersen, R. M. Sorensen, S. Quartel, and N. Vinther, 2005. Intertidal beach change during storm conditions; Egmond, The Netherlands, Marine Geology, 218: 65-80 https://doi.org/10.1016/j.margeo.2005.04.001
  2. Aarninkhof, S., I. L. Turner, T. D. T. Dronkers, C. Mark, and N. Leann, 2003. A video-based technique for mapping intertidal beach bathymetry. Coastal Engineering, 49: 275-289 https://doi.org/10.1016/S0378-3839(03)00064-4
  3. Bradley D. M., A. D. Mark, and A. H. David, 2001. Measurements of the response of a coastal inlet using video monitoring techniques, Marine Geology, 175: 251-272 https://doi.org/10.1016/S0025-3227(01)00144-X
  4. Bright Janssen-Stelder, 2000. The effect of different hydrodynamics conditions on the morphodynamics of a tidal mudflat in the Dutch Wadden Sea. Continental Shelf Research, 20: 1461-1478 https://doi.org/10.1016/S0278-4343(00)00032-7
  5. Holand K. T., R. A. Holman, T. C. Lippmann, J. Stanley, and P. Nathaniel, 1997. Practical use of video imagery in nearshore oceanographic field studies. IEEE Journal of Oceanic Engineering, 22: 81-92 https://doi.org/10.1109/48.557542
  6. Mikhail E. M. and J. S. Bethel, 2001. Intorduction to modern photogrammetry. New York, John Wiley & Sons, Inc., 93p
  7. Nathaniel G. P. and R. A. Holman, 1997. Intertidal beach profile estimation using video images. Marine Geology, 140: 1-24 https://doi.org/10.1016/S0025-3227(97)00019-4
  8. O’Brien, D. J., R. J. S. Whitehouse, and A. Cramp, 2000. The cyclic development of a macrotidal mudflat on varying time scales. Continental Shelf Research, 20: 1593-1619 https://doi.org/10.1016/S0278-4343(00)00039-X
  9. Roberts W., P. H. Le, and R. J. S. Whitehouse, 2000. Investigation using simple mathematical models of the effect of tidal currents and wave son the profile shape of intertidal mudflats. Continental Shelf Research, 20: 1079-1097 https://doi.org/10.1016/S0278-4343(00)00013-3
  10. Kim T. and S. Park, 2006. Study on Intertidal flat topography observation using camera images. Journal of the Korean Society of Oceanogrphy, 11(4): 145-151
  11. Wright, L. D., P. Nielsen, A. D. Short, and M. O. Green, 1982. Morphodynamics of a macrotidal beach. Marine Geology, 50: 97-128 https://doi.org/10.1016/0025-3227(82)90063-9
  12. Whitehouse R. J. S., P. Bassoullet, K. R. Dyer, H. J. Mitchener, and W. Roberts, 2000. The influence of bedforms on flow and sediment transport over intertidal mudflats. Continental Shelf Research, 20: 1099-1124 https://doi.org/10.1016/S0278-4343(00)00014-5