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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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where 1 is the two-by-two identity matrix, 0 is the two-by-two zero matrix<br />

and<br />

c= (41)<br />

c=<br />

Expansion <strong>of</strong> the determinant by c<strong>of</strong>actors leads to<br />

det (A A_-e) = det c det C<br />

(43)<br />

Therefore, the roots <strong>of</strong> equation (39) may be found from<br />

det = 0<br />

(44)<br />

and<br />

det C = 0 (45)<br />

It is interesting to note that advection has no effect on the characteristic<br />

directions. The existence and direction <strong>of</strong> characteristic curves<br />

depend only on properties <strong>of</strong> the yield curve and flow rule. Perhaps it is<br />

not surprising that the water stress, Coriolis force, and other applied body<br />

forces have no effect; but since the velocity gradient components appear in<br />

the advection terms, it seems surprising that characteristic curves may be<br />

found without considering this term.<br />

The elements <strong>of</strong> the matrix arise from the stress divergence term in<br />

the momentum balance equations. Therefore, we call the directions obtained<br />

by satisfying equation (44) the stress characteristics. Also, we<br />

12 7

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