Oceanography > Issues > Archive > Volume 25, Issue 1

2012, Oceanography 25(1):180–181, http://dx.doi.org/10.5670/oceanog.2012.15

Turbulence Observations in a Buoyant Hydrothermal Plume on the East Pacific Rise

Authors | First Paragraph | Full Article | Citation | References


Andreas M. Thurnherr | Division of Ocean and Climate Physics, Lamont-Doherty Earth Observatory, Columbia University, Palisades, NY, USA

Louis C. St. Laurent | Physical Oceanography Department, Woods Hole Oceanographic Institution, Woods Hole, MA, USA


First Paragraph

Hot vent fluid enters the ocean at high-temperature hydrothermal vents, also known as black smokers. Because of the large temperature difference between the vent fluid and oceanic near-bottom waters, the hydrothermal effluent initially rises as a buoyant plume through the water column. During its rise, the plume engulfs and mixes with background ocean water. This process, called entrainment, gradually reduces the density of the rising plume until it reaches its level of neutral buoyancy, where the plume density equals that of the background water, and it begins to spread along a surface of constant density. (For a much more detailed discussion of buoyant hydrothermal plumes, see Di Iorio et al., 2012, in this issue.)


Full Article

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Thurnherr, A.M., and L.C. St. Laurent. 2012. Turbulence observations in a buoyant hydrothermal plume on the East Pacific Rise. Oceanography 25(1):180–181, http://dx.doi.org/10.5670/oceanog.2012.15.



Di Iorio, D., J.W. Lavelle, P.A. Rona, K. Bemis, G. Xu, L.N. Germanovich, R.P. Lowell, and G. Genc. 2012. Measurements and models of heat flux and plumes from hydrothermal discharges near the deep seafloor. Oceanography 25(1):168–179, http://dx.doi.org/10.5670/oceanog.2012.14.

Jackson, P.R., J.R. Ledwell, and A.M. Thurnherr. 2010. Dispersion of a tracer on the East Pacific Rise (9°N to 10°N), including the influence of hydrothermal plumes. Deep Sea Research Part I 57:37–52, http://dx.doi.org/10.1016/j.dsr.2009.10.011.

Lupton, J. 1998. Hydrothermal helium plumes in the Pacific Ocean. Journal of Geophysical Research 103:15,853–15,868, http://dx.doi.org/10.1029/98JC00146.

McGillicuddy, D.J., J.W. Lavelle, A.M. Thurnherr, V.K. Kosnyrev, and L.S. Mullineaux. 2010. Larval dispersion along an axially symmetric mid-ocean ridge. Deep Sea Research Part I 57:880–892, http://dx.doi.org/10.1016/j.dsr.2010.04.003.

Thurnherr, A.M., and L.C. St. Laurent. 2011. Turbulence and diapycnal mixing over the East Pacific Rise crest near 10°N. Geophysical Research Letters 38, L15613, http://dx.doi.org/10.1029/2011GL048207.

Thurnherr, A.M., J.R. Ledwell, J.W. Lavelle, and L.S. Mullineaux. 2011. Hydrography and circulation near the crest of the East Pacific Rise between 9° and 10°N. Deep Sea Research Part I 58:365–376, http://dx.doi.org/10.1016/j.dsr.2011.01.009.