A salt flux model for salinity change through ice production in the Greenland Sea, and its relationship to winter convection
A salt flux model which incorporates ice formation, advection and melt, as well as time-dependent brine drainage from frazil-pancake ice, has been developed for the central Greenland Sea in winter. Information from ice drifting buoys suggests that this region can be thought of as similar to a latent...
Published in: | Journal of Geophysical Research |
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Main Authors: | , |
Format: | Article in Journal/Newspaper |
Language: | English |
Published: |
2003
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Subjects: | |
Online Access: | https://pure.uhi.ac.uk/en/publications/c3c19abb-754d-41ec-8559-497e1b015889 https://doi.org/10.1029/2001JC001099 |