HR: 0800h
AN: OS21C-1250 [Abstracts]
TI: Internal tides and boundary mixing imaged on the Norwegian continental slope
AU: * Holbrook, W S
EM: steveh@uwyo.edu
AF: University of Wyoming, Dept. of Geology and Geophysics
#3006, laramie, WY 82072-3006
United States
AU: Fer, I
EM: ilker.fer@gfi.uib.no
AF: Bjerknes Centre for Climate Research, Geofysisk institutt
All‚gaten 70, Bergen, N-5007
Norway
AU: Nandi, P
EM: pnandi@uwyo.edu
AF: University of Wyoming, Dept. of Geology and Geophysics
#3006, laramie, WY 82072-3006
United States
AU: Paramo, P
EM: paramo@uwyo.edu
AF: University of Wyoming, Dept. of Geology and Geophysics
#3006, laramie, WY 82072-3006
United States
AB:
Boundary mixing on continental slopes and other topographic features may
help maintain the ocean's stratification by converting low-mode internal
wave energy into increased potential energy via turbulence, but existing
observations are too sparse to assess whether this process is sufficiently
widespread to affect global balances. Here we present a new method for
identifying and quantifying internal wave processes in the ocean by acoustic
imaging. Seismic reflection images of thermohaline finestructure in the
Norwegian Sea that show semidiurnal (M2) internal waves and associated zones of turbulent disruption of finestructure on the
continental slope of Norway. The disrupted zone occur at water depths of ~500-650 m, where the slope is critical to M2
internal waves and the water column is highly stratified.
Wavenumber spectra calculated from finestructure displacements in the
disrupted zones show enhanced energy levels, relative to both open-ocean
finestructure and the Garrett-Munk spectrum. These results imply that
seismic reflection profiling can remotely detect internal waves, identify
the locations and dimensions of sites of boundary mixing, and provide
quantitative estimates of internal wave energy in the ocean.
DE: 4544 Internal and inertial waves
DE: 4594 Instruments and techniques
DE: 0910 Data processing
DE: 0930 Oceanic structures
SC: Ocean Sciences [OS]
MN: 2004 AGU Fall Meeting