Flow in the Endeavour Segment's Rift Valley

From García-Berdeal, et al. (2006).

Objectives:
- Characterization of the near bottom boundary layer (BBL) of low-temperature hydrothermal vents, including the vertical turbulent heat flux
- Physics and observations of tidal currents within the axial valley and the resulting variability in high temperature plumes
- The implications of currents and turbulence to larval dispersion and retention.
Investigators
Susan Hautala (University of Washington)
Paul Johnson (University of Washington)
Irene García-Berdeal (University of Washington)
Matt Pruis (NorthWest Research Associates, Redmond)
Tor Bjorklund (University of Washington)
Leif Thomas (Stanford)
Data
Plots and data for measurements of diffuse heat flux and flow in the turbulent benthic boundary layer
Publications
- Hautala, S., H. P. Johnson, M. Pruis, I. Garcia-Berdeal, T. Bjorklund (2012). Low-temperature hydrothermal plumes in the near-bottom boundary layer at Endeavour Segment, Juan de Fuca Ridge. Oceanography 25: 192-195
- García-Berdeal, I. (2006). Hydrography and flow in the axial valley of the Endeavour Segment: Implications for larval dispersal. PhD Dissertation, University of Washington, Seattle.
- Garcia Berdeal, I., S. L. Hautala, Leif N. Thomas and H. P. Johnson (2006). Vertical structure of time-dependent currents in a mid-ocean ridge axial valley. Deep-Sea Res. 53: 367-386.
- Pruis, M.J. (2004). Energy and volume flux into the deep ocean: Examining diffuse hydrothermal systems. PhD Dissertation, University of Washington, Seattle.
- Johnson, H. P., S. L. Hautala, M. A. Tivey, C. D. Jones, J. Voight, M. Pruis, I. Garcia-Berdeal, L. A. Gilbert, T. Bjorklund, W. Fredericks, J. Howland and the Thermal Grid Scientific Party (2002). A systematic examination of hydrothermal circulation: Endeavour Segment, Juan de Fuca Ridge. EOS Transactions of the American Geophysical Union 83: 73 and 78.
Funding
National Science Foundation
University of Washington Royalty Research Fund