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Published byLoreen Hancock Modified over 9 years ago
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Boundary Layer Velocity Structure in a Coldwater Coral Area of Haddock Channel, Southwest Grand Banks William Fowler MSc. Candidate Environmental Science Memorial University of Newfoundland
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Large Gorgonian Distribution Coldwater Coral off Newfoundland and Labrador, WWF 2007
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Characterization of Local Current Regime Corals occurring on the bottom in deep water are located in the benthic boundary layer Layer extends above seafloor anywhere from 5-20 meters Dr. Len Zedel / Dr. Evan Edinger, ROPOS 2007
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Boundary Layers Idealized boundary layer Bottom drag, sea floor roughness important factor NASA 2008
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Methods ROPOS/Hudson 2007 Cruise Survey of deepwater coral Multiple sites along slope of continental shelf 2008 Dr. Evan Edinger
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ADCP
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Profiler 1: Area without Coral Dr. Len Zedel / Dr. Evan Edinger, ROPOS 2007
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Current Profiler 2: Coral Thicket Dr. Len Zedel / Dr. Evan Edinger, ROPOS 2007
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Deployment Parameters Depth 700 meters 1 profile every 30 seconds Uncertainty in velocity time series ~ 0.5 cm/s Profiling over 4 meters 1 meter cell size
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Location of ADCP in Coral Thicket (site 2)
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ROPOS Transact and location of coral
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Mean normalized velocity profile
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Comparison of Site 1 and 2
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Directional Velocity Profile: Inst. 1
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Coral Thicket varies relative to site 1
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Directional Velocity Profile w/ time series
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Directional subplots Inst. 1 shown (use inst. 2 plots in presentation)
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