AIDJEX Bulletin #40 - Polar Science Center - University of Washington
AIDJEX Bulletin #40 - Polar Science Center - University of Washington
AIDJEX Bulletin #40 - Polar Science Center - University of Washington
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the stress characteristics, S a = 1,2. Since C is singular, equation<br />
-a ’ -a<br />
(106) is meaningless. However, our intuition leads us to believe that the<br />
model should not change dramatically when a normal flow rule is introduced.<br />
It also seems that the characteristic analysis should not become invalid.<br />
It is felt further that the governing equations possess finite limits. Our<br />
future efforts are aimed at determining these limits.<br />
CONCLUSION<br />
In the introduction to this paper five goals <strong>of</strong> this work were stated.<br />
Although no one goal has been met entirely, there has been substantial,<br />
progress toward all <strong>of</strong> them.<br />
Our understanding <strong>of</strong> discontinuities has improved. We have determined<br />
that the differential equations governing quasi-steady, rigid-plastic ice<br />
models cannot be simply characterized because theymaybelocallyhyperbolic,<br />
parabolic, or elliptic, depending on the state <strong>of</strong> stress (or stretching) at<br />
each point. The ratio <strong>of</strong> shearing to dilating ocntrols the character <strong>of</strong><br />
the system. If shearing predominates ( ~ / < 48 < 3?r/4), the system is hyperbolic<br />
and two distinct real characteristic directions exist, But when<br />
dilating is predominant (either opening, 8 < ~/4, or closing, 8 > 3~/4),<br />
the system is elliptic and no real characteristic directions exist. In the<br />
cases <strong>of</strong> uniaxial extension (e = ~/4) and uniaxial contraction (0 = 3~/4),<br />
the system is parabolic and one real characteristic direction occurs. The<br />
crucial point to be made is that the plasticity model can admit discontinuous<br />
solutions whenever real characteristic curves exist. This property is<br />
dramatically different from other models such as viscous models which are<br />
always elliptic during quasi-steady flow. We believe discontinuities are<br />
necessary to allow the explanation <strong>of</strong> such diverse features as spatially<br />
smooth velocity fields, shear ridging, and large leads formed within the<br />
pack ice. We know <strong>of</strong> no model other than a plastic model that allows a<br />
natural representation <strong>of</strong> all these features.<br />
It is anticipated that interpretation <strong>of</strong> numerical solutions will be<br />
enhanced by knowing the conditions under which discontinuities may appear.<br />
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