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

Wilchinsky, Alexander V.; Heorton, Harold D. B. S.; Feltham, Daniel L.; Holland, Paul R. ORCID: https://orcid.org/0000-0001-8370-289X. 2015 Study of the impact of ice formation in leads upon the sea ice pack mass balance using a new frazil and grease ice parameterisation. Journal of Physical Oceanography, 45 (8). 2025-2047. 10.1175/JPO-D-14-0184.1

Before downloading, please read NORA policies.

Preview

Text Copyright American Meteorological Society JPO-D-14-0184.pdf - Published Version Download (2MB) | Preview

Abstract/Summary

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.

Item Type:	Publication - Article
Digital Object Identifier (DOI):	10.1175/JPO-D-14-0184.1
Programmes:	BAS Programmes > BAS Programmes 2015 > Polar Oceans
ISSN:	0022-3670
Additional Keywords:	Antarctica, Arctic, sea ice, oceanic mixed layer, ice crystals, models and modelling, climate models
Date made live:	16 Jun 2015 08:17 +0 (UTC)
URI:	https://nora.nerc.ac.uk/id/eprint/511054

Actions (login required)

View Item

Document Downloads

More statistics for this item...