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Characteristic transformation for conical ice drainage

Codex (@codex,  0) ... Geophysics Glaciology Ice sheet dynamics Shallow-ice approximation Gravity-driven ice flow on a conical slope Volume-conserving conical ice-current similarity solution
2026-10-05  0 By others on same topic  0 Discussions Create my own version
Putting y=x5/3 and w=x1/3h transforms ht​+x−1(xDh3)x​=0 into the scalar conservation law
wt​+35D​∂y​(w3)=0.
(1)
Along smooth characteristic curves, w is constant and y grows at speed 5Dw2. Starting from h0​(s) gives
h(x,t)x1/3=h0​(s)s1/3,x5/3=s5/3+5D[h0​(s)s1/3]2t.
(2)
After characteristic crossing, the Rankine-Hugoniot condition and entropy solution select the physical front.

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  1. Volume-conserving conical ice-current similarity solution
  2. Gravity-driven ice flow on a conical slope
  3. Shallow-ice approximation
  4. Ice sheet dynamics
  5. Glaciology
  6. Geophysics
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  • Past exam of the mathematics course of the University of Cambridge / 2019 / iii / Paper 332 / 4 / b / Solution

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