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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 />

147

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