Study of the impact of ice formation in leads upon the sea ice pack mass balance using a new frazil and grease ice parameterisation

• Published in: Journal of Physical Oceanography
• Main Authors: Wilchinsky, Alexander V., Heorton, Harold D. B. S., Feltham, Daniel L., Holland, Paul R.
• Format: Article in Journal/Newspaper
• Language: English
• Published: American Meteorological Society 2015
• Subjects: Arctic; Antarctic; The Antarctic; Antarc*; ice pack; Sea ice
• Online Access: http://nora.nerc.ac.uk/id/eprint/511054/; https://nora.nerc.ac.uk/id/eprint/511054/1/JPO-D-14-0184.pdf; https://doi.org/10.1175/JPO-D-14-0184.1

Leads are cracks in sea ice that often form due to deformation. During winter months leads expose the ocean to the cold atmosphere resulting in supercooling and the formation of frazil ice crystals within the mixed layer. Here we investigate the role of frazil ice formation in leads on the mass balance of the sea ice pack through the incorporation of a new module into the Los Alamos sea ice model (CICE). The frazil ice module considers a initial cooling of leads followed by a steady state formation of uniformly distributed single size frazil ice crystals that precipitate to the ocean surface as grease ice. The grease ice is pushed against one of the lead edges by wind and water drag that we represent through a variable collection thickness for new sea ice. Simulations of the sea ice cover in the Arctic and Antarctic are performed and compared to a model that treats leads the same as the open ocean. The processes of ice formation in the new module slows down the refreezing of leads resulting in an longer period of frazil ice production. The fraction of frazil-derived sea ice increases from 10% to 50%, corresponding better to observations. The new module has higher ice formation rates in areas of high ice concentration and thus has a greater impact within multiyear ice than it does in the marginal seas. The thickness of sea ice in the central Arctic increases by over 0.5 m whereas within the Antarctic it remains unchanged.