Tidal scour

Tidal scour is “sea-floor erosion caused by strong tidal currents resulting in the removal of inshore sediments and formation of deep holes and channels”.[1] Examples of this hydrological process can be found globally.[2][3][4] Two locations in the United States where tidal scour is the predominant shaping force is the San Francisco Bay and the Elkhorn Slough.[2][5][6] Tidal force can also contribute to bridge scour.[2]

Historical Perspective and Relevance

Research on tidal scour is largely centered at Elkhorn Slough in California.[2] The slough was directly exposed to tidal flux beginning in 1947 with the creation of the Moss Landing Harbor.[2][5] Multiple studies have been done on the slough since tidal exposure to catalog the morphological change and determine how long it will take for the system to reach equilibrium.[2][5]

Elkhorn Slough is the focus of many tidal scour studies. Tidal scour became prevalent with the creation of the Moss Landing Harbor seen toward the bottom of the image.

Formation

Tidal Scours are formed in tide-dominated deltas and estuaries with the changing of the tide. As the tide changes from low to high or high to low, water is transported through the channel taking sediment with it. With increasing erosion, there is increasing tidal volume creating a self-perpetuating system.[2] Tidal scour is most apparent when a barrier is breached due to natural or anthropogenic forcing.[2][3]

Anatomy

Bathymetry

Tidal scour can be determined by looking at the change in bathymetry over time. Bathymetry of tidal channels is determined using multi-beam sonar or LiDAR. By comparing cross-sections of channel bathymetry over several years and at various distances in the tidal channel, the amount of tidal scour can be quantified.[2][4][7]

Grain Size Distribution

Sediment grab samples show that in areas demonstrating tidal scour, there is an increase in grain size from surrounding areas.[5]

Ecological Significance

With direct influence from the Ocean, slough morphology can change significantly making it difficult for native species to persist.[2] This can be seen in:

See also

References
  1. Parker, Sybil (1994). McGraw Hill dictionary of scientific and technical terms. New York: McGraw-Hill. ISBN 978-0-07-113584-9.
  2. Dean, Edwin (2003). "Tidal Scour in Elkhorn Slough, California: A Bathymetric Analysis" (PDF). Seafloor Mapping Lab, USC Monterey Bay. USC Monterey Bay. Retrieved 15 December 2019.
  3. Lewis, Keith; Carter, Lionel; Davey, Fred (1994). "The Opening of Cook Strait: Interglacial tidal scour and aligning basins at a subduction to transform plate edge". Marine Geology. 116 (3–4): 293–312. doi:10.1016/0025-3227(94)90047-7. Retrieved 15 December 2019.
  4. Shaw, John; Todd, Brian; Li, Michael; Wu, Yongsheng (2012). "Anatomy of the tidal scour system at Minas Passage, Bay of Fundy, Canada". Marine Geology. 323–325: 123–134. doi:10.1016/j.margeo.2012.07.007.
  5. Malzonen, Christopher (1999). "Tidal scour and its relation to erosion and sediment transport in Elkhorn Slough". Master's Theses. Retrieved 15 December 2019.
  6. Silberstein 1989 M, Campbell E. 1989. Elkhorn Slough. Monterey, CA: Monterey Bay Aquarium. 64 p.
  7. McMullen, Katherine; Poppe, Lawrence; Parker, Castle (2015). "Character, distribution, and ecological significance of storm wave-induced scour in Rhode Island Sound, USA". Geo-Marine Letters. 35 (2): 135–144. doi:10.1007/s00367-014-0392-0. hdl:1912/7246.
  8. "Caspian terns: the world's biggest tern nests at Elkhorn Slough!". Elkhorn Slough National Estuarine Research Reserve (ESNERR). 2001. Retrieved 15 December 2019. (dead link)
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