Abstract
The Antarctic sea ice zone undergoes one of the greatest seasonal surface
changes on Earth, with an annual change in extent of around 15 × 10
6 km 2 . This ice, and its
associated snow cover, plays a number of important roles in the
ocean-atmosphere climate system: the high albedo ice cover restricts surface
absorption of solar radiation and acts as a barrier to the exchange of mass
and energy between the ocean and atmosphere, and salt rejected by the growing
ice cover affects the ocean structure and circulation. Additionally, a number
of sea ice feedback processes have the potential to play an important role in
climate change.
The extent to which a sea ice cover modifies ocean-atmosphere interaction is
primarily determined by the thickness and concentration of the ice, but these
themselves are determined by ocean and atmospheric interaction. The thickness
distribution of the pack is determined by both thermodynamic and dynamic
processes: most important at the geophysical scale are the dynamic processes
of ice drift and deformation, and of lead formation. Compared to the ice cover
in the central Arctic Basin, the Antarctic sea ice is highly mobile. Drifting
buoy studies show that the Antarctic pack can move at speeds of up to 60 km
per day or greater, and that around most of the Antarctic coast, the drift of
the pack ice is generally divergent, with divergence rates of 10% or
more per day being observed under some circumstances. Consequently there is
generally some open water within the Antarctic pack and much of the total ice
mass forms by rapid growth within these areas. This influences the crystal
structure of the ice and results in a considerable portion of the Antarctic
pack (up to 25% in spring-time) having a thickness of less than 0
· 3 m. In general much of the Antarctic sea ice only grows
thermodynamically to about 0·5 m thick, with thickness increases beyond
that resulting from the deformational processes of rafting and ridge-building.
Subject
General Physics and Astronomy
Cited by
15 articles.
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