William M Connolley wrote:
> On Fri, 10 Aug 2007, Eric Swanson wrote:
> > As the sea-ice extent declines, it's thickness also decreases.  I
> > think it's likely that the thickness will decline so much that there
> > will be the chance of a mechanical failure, even before the extent
> > could actually reaches zero.   The result could look much like the
> > breakup of the Larson B ice shelf along the Antarctic Peninsula, which
> > was sudden and spectacular .
>
> This is unlikely. Sea ice has essentially no strength in tension anyway.

Looking about, I found some references to various models for sea-ice
strength, i.e., rheology.  An early modeling approach by Hibler used a
viscous-plastic assumption, which has been used by some ocean model
builders.  There appear to be other models based on an elastic
assumption, such as this one:

David M. Holland, "A 1-D elastic-plastic sea-ice model solved with an
implicit Eulerian-Lagrangian method", Ocean Modelling Volume 17, Issue
1, 2007, Pages 1-27

Either way, it would seem that the resistance to motion would be
greater for thicker multi-year ice than for first year ice.  It's the
potential for an increase in motion that I think would be important.
To begin with, if the sea-ice is no longer bound to fast ice along the
coast lines, surely it would move faster.    Here's a model study
which uses an elastic-plastic model:

http://efdl.cims.nyu.edu/publications/summer_students/mazover_landfast_05.pdf

I think their point about the permanence of landfast ice is important,
since we know it exists and isn't easily dislodged.  This suggests
that the tensile strength of sea-ice away from the coast may also be
important.

E. S.


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