Articles | Volume 12, issue 2
Ocean Sci., 12, 507–515, 2016
Ocean Sci., 12, 507–515, 2016

Research article 06 Apr 2016

Research article | 06 Apr 2016

Turbulent heat transfer as a control of platelet ice growth in supercooled under-ice ocean boundary layers

Miles G. McPhee et al.

Cited articles

Craven, M., Carsey, F., Behar, A., Matthews, J., Brand, R., Elcheikh, A., Hall, S., and Treverrow, A.: Borehole imagery of meteoric and marine ice layers in the Amery Ice Shelf, East Antarctica, J. Glaciol., 51, 75–84,, 2005.
Craven, M., Warner, R. C., Galton-Fenzi, B. K., Herraiz-Borreguero, L., Vogel, S. W., and Allison, I.: Platelet ice attachment to instrument strings beneath the Amery Ice Shelf, East Antarctica, J. Glaciol., 60, 383–393,, 2014.
Crawford, G., Padman L., and McPhee, M. G.: Turbulent mixing in Barrow Strait, Cont. Shelf Res., 19, 205–245,, 1999.
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Dayton, P. K., Robilliard, G. A., and DeVries, A. L.: Anchor ice formation in McMurdo Sound, Antarctica, and its biological effects, Science, 163, 274–276, 1969.
Short summary
Measurements of turbulent heat fluxes in tidally modulated flow of supercool seawater under Antarctic land-fast sea ice show that turbulent heat exchange at the ocean–ice boundary is characterized by the product of friction velocity and (negative) water temperature departure from freezing. Also, the conditions cause platelet ice growth to form on the underside of the sea ice which increases the hydraulic roughness (drag) of fast ice compared to ice without platelets.