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GEOPHYSICAL RESEARCH LETTERS,
VOL. 33,
L19313,
doi:10.1029/2006GL027211,
2006
Entrainment and bending in a major hydrothermal plume, Main Endeavour Field, Juan de Fuca Ridge
Peter A. Rona
Department of Geological Sciences, Rutgers–State University of New Jersey, New Brunswick, New Jersey, USA
Karen G. Bemis
Department of Geological Sciences, Rutgers–State University of New Jersey, New Brunswick, New Jersey, USA
Christopher D. Jones
Applied Physics Laboratory, University of Washington, Seattle, Washington, USA
Darrell R. Jackson
Applied Physics Laboratory, University of Washington, Seattle, Washington, USA
Kyohiko Mitsuzawa
Japan Agency for Marine-Earth Science and Technology, Yokosuka, Japan
Deborah Silver
Department of Geological Sciences, Rutgers–State University of New Jersey, New Brunswick, New Jersey, USA
Abstract
We measure expansion rate and bending in a 23-hour time series of acoustic images of the lower 25 m section of a buoyant hydrothermal
plume rising from Grotto vent in the Main Endeavour Field, Juan de Fuca Ridge. We then calculate entrainment coefficient,
the constant of proportionality relating mean inflow velocity at the plume edge to maximum mean upward velocity within the
plume. The plume section alternately bends southwest at relatively high inclinations (37°) and northeast at lower inclinations
at irregular intervals twice during this time period, apparently driven by current reversals in the mixed semi-diurnal tidal
cycle. The measured expansion rates (0.11–0.25 m/m) and calculated entrainment coefficients (0.07–0.18) are directly proportional
to the degree of bending (R2 = 0.75). The loss of buoyancy flux related to enhanced mixing in a stratified environment during bending may contribute to
reduction of potential rise height consistent with predicted (∼400 m) and measured (300–350 m) plume tops.
Received 13
June
2006;
accepted 31
August
2006;
published 14
October
2006.
Index Terms: 3017 Marine Geology and Geophysics: Hydrothermal systems (0450, 1034, 3616, 4832, 8135, 8424); 4568 Oceanography: Physical: Turbulence, diffusion, and mixing processes (4490); 4832 Oceanography: Biological and Chemical: Hydrothermal systems (0450, 1034, 3017, 3616, 8135, 8424).
Read Full Article (file size: 450936 bytes) Cited by
Citation: Rona, P. A., K. G. Bemis, C. D. Jones, D. R. Jackson, K. Mitsuzawa, and D. Silver
(2006),
Entrainment and bending in a major hydrothermal plume, Main Endeavour Field, Juan de Fuca Ridge,
Geophys. Res. Lett.,
33,
L19313,
doi:10.1029/2006GL027211.
Copyright 2006 by the American Geophysical Union.
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