Habitat characterization of a tidal energy site using an ROV: Overcoming difficulties in a harsh environment

Abstract The Snohomish County Public Utility District (Snohomish) in Washington State USA has undertaken a tidal turbine site investigation at Admiralty Head, the entrance into the Puget Sound, to determine the feasibility of installing two energy conversion plants that will supply electrical power to the local grid. This site is close to shore and to major metropolitan areas that can benefit from this cleanly generated power. Large tidal exchanges take place at this site and can provide predictable and sustainable tidal energy. As part of the permitting process Snohomish has undertaken a seafloor investigation to determine the habitat characteristics of the seafloor and inform the appropriate location for the turbines' placement. In 2010, to assess habitat types multibeam echosounder (MBES) images were produced and ground-truth video surveys using an ROV were undertaken with the requirement that little disturbance occurs to the seafloor. Collection of these data was challenging as the highly dynamic oceanographic and geologic (tectonic) environment made it difficult to undertake in situ observations of the seafloor. Strong tidal currents, even during predicted slack tides, forced new thinking on how data should be collected in order to evaluate the seafloor substrate, habitats and ecology in light that a statistically methodology could not be accomplished, or if indeed a statistical analysis was necessary at all. Additional information on tidal currents has been gathered since these surveys, which should aid in the future collection of data, although the underlying questions about the possibility of, and need for, a statistical analysis remain. Extensive video assessment was needed to produce a map that could exhibit habitat types. This was attempted by focusing on the geology of the seafloor and selecting common organisms, such as sessile and encrusting fauna (e.g., sea anemones, barnacle fields, crinoids) and epifauna (e.g., sea stars) to relate to substrate types. Heavily encrusted and lightly encrusted substrates were mapped to show areas where sediment is presently being transported through the area. ROV line- or timed-transects to count biota appears not to be necessary to obtain information needed to validate marine benthic habitat types. Rather, general observational transects and more stabilized in situ observational stations used for close examination of the biota and measurement of the substrate is recommended

[1]  J. Barrie,et al.  Large-scale sedimentary bedforms and sediment dynamics on a glaciated tectonic continental shelf : Examples from the Pacific margin of Canada , 2009 .

[2]  A. Moore,et al.  A Tsunami About 1000 Years Ago in Puget Sound, Washington , 1992, Science.

[3]  P. Mozzi,et al.  Middle Terrace Deposits of the Tagus River in Alpiarça, Portugal, in Relation to Early Human Occupation , 2000, Quaternary Research.

[4]  J. Barrie,et al.  Rapid sea-level change and coastal evolution on the Pacific margin of Canada , 2002 .

[5]  Deidre Sullivan,et al.  A classification scheme for deep seafloor habitats , 1999 .

[6]  E. B. Leopold,et al.  Holocene Relative Sea Level Changes along the Seattle Fault at Restoration Point, Washington , 2000, Quaternary Research.

[7]  D. Easterbrook Advance and Retreat of Cordilleran Ice Sheets in Washington, U.S.A. , 2007 .

[8]  R. Bucknam,et al.  Late Holocene earthquakes on the Toe Jam Hill fault, Seattle fault zone, Bainbridge Island, Washington , 2003 .

[9]  C. Wentworth Method of Computing Mechanical Composition Types in Sediments , 1929 .

[10]  Samuel Y. Johnson,et al.  Geologic evidence of earthquakes at the Snohomish delta, Washington, in the past 1200 yr , 2001 .

[11]  Robert E. Pacunski,et al.  Conducting Visual Surveys with a Small ROV in Shallow Water , 2008 .

[12]  Mary M. Yoklavich,et al.  Multiscale habitat associations of deepwater demersal fishes off central California , 2007 .

[13]  R. Bucknam,et al.  Abrupt Uplift Within the Past 1700 Years at Southern Puget Sound, Washington , 1992, Science.

[14]  B. Sherrod,et al.  Land-level changes from a late Holocene earthquake in the northern Puget Lowland, Washington , 2004 .

[15]  H. Williams,et al.  Stratigraphic and Microfossil Evidence for Late Holocene Tsunamis at Swantown Marsh, Whidbey Island, Washington , 2000, Quaternary Research.

[16]  R. Macdonald,et al.  Distribution and Cycling of Suspended Particles Inferred from Transmissivity in the Strait of Georgia, Haro Strait and Juan de Fuca Strait , 2006 .

[17]  J. Clague,et al.  Quaternary Geology of the Canadian Cordillera , 1989 .

[18]  A. Nelson,et al.  Multiple sources for late-Holocene tsunamis at Discovery Bay, Washington State, USA , 2002 .

[19]  S. C. Porter,et al.  Radiocarbon Age Constraints on Rates of Advance and Retreat of the Puget Lobe of the Cordilleran Ice Sheet during the Last Glaciation , 1998, Quaternary Research.