Estimation of ice shelf melt rate in the presence of a thermohaline staircase

Diffusive convection–favorable thermohaline staircases are observed directly beneath George VI Ice Shelf, Antarctica. A thermohaline staircase is one of the most pronounced manifestations of double-diffusive convection. Cooling and freshening of the ocean by melting ice produces cool, freshwater abo...

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Bibliographic Details
Published in:Journal of Physical Oceanography
Main Authors: Kimura, Satoshi, Nicholls, Keith W., Venables, Emily
Format: Article in Journal/Newspaper
Language:English
Published: American Meteorological Society 2015
Subjects:
Online Access:http://nora.nerc.ac.uk/id/eprint/508647/
https://nora.nerc.ac.uk/id/eprint/508647/1/JPO-D-14-0106.pdf
https://doi.org/10.1175/JPO-D-14-0106.1