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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.

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Presentation on theme: "Boundary Layer Velocity Structure in a Coldwater Coral Area of Haddock Channel, Southwest Grand Banks William Fowler MSc. Candidate Environmental Science."— Presentation transcript:

1 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

2 Large Gorgonian Distribution Coldwater Coral off Newfoundland and Labrador, WWF 2007

3 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

4 Boundary Layers Idealized boundary layer Bottom drag, sea floor roughness important factor NASA 2008

5 Methods ROPOS/Hudson 2007 Cruise Survey of deepwater coral Multiple sites along slope of continental shelf 2008 Dr. Evan Edinger

6 ADCP

7 Profiler 1: Area without Coral Dr. Len Zedel / Dr. Evan Edinger, ROPOS 2007

8 Current Profiler 2: Coral Thicket Dr. Len Zedel / Dr. Evan Edinger, ROPOS 2007

9 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

10 Location of ADCP in Coral Thicket (site 2)

11 ROPOS Transact and location of coral

12 Mean normalized velocity profile

13 Comparison of Site 1 and 2

14 Directional Velocity Profile: Inst. 1

15 Coral Thicket varies relative to site 1

16 Directional Velocity Profile w/ time series

17 Directional subplots Inst. 1 shown (use inst. 2 plots in presentation)


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