crevprop.crevasse¶
2021-2024 J. Mejia
- Model Geometry
→ x
↓ z
- ‾‾‾‾⎡‾‾‾‾ /‾‾‾‾‾‾‾‾‾ ⎤
⎜ / ⎟ ⎜ <– D(z) –>/ ⎟ ⎜ / ⎟ d -——-/ <— water surface ⎦ ⎜ wwwwww/ ⎜ wwww/ ⎜ ww/ ⎣ crevasse /
depth
STRESS INTENSITY FACTOR For a fracture to propagate
KI >= KIC
stress @ crev tip must >= fracture toughness of ice where KI is the stress intensity factor which describes the stresses at the fracture’s tip the material’s fracture toughness (KIC) STRESS INTENSITY FACTOR For a fracture to propagate
KI >= KIC
stress @ crev tip must >= fracture toughness of ice where KI is the stress intensity factor which describes the stresses at the fracture’s tip the material’s fracture toughness (KIC) Syntax from van der Veen dw = depth to water ( or water depth) = distance from ice surface to
the top of the water column within crevasee
d = crevasse depth = crevasse depth below ice surface b = water height above crevasse tip dw = d - b
Find crack geometry and shape given water input(R, b, Nyrs) and
- background stress(sigmaT: + compression, - tensile) and physical
constants(poissons ratio, shear modulus)
Takes into account 1. Elastic opening(based on Krawczynski 2009) 2. Viscous closure(based on Lilien Elmer results) 3. Refreezing rate(diffusion and temperature gradient at sidewalls)
Functions
| empirical density-depth relationship from Paterson 1994 |
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| Helper to handle indices and logical indices of NaNs. |
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Classes
| Crevasse formed considering elastic, creep, and refreezing |