Crevasse Penetration Tensile Stress Calculator
RestrictedNyezerowatercrevasse-depth2σ/(ρg) stressbalance,unrealisticuniformtensionandnowaterpressureexplicit,not crackmechanicsor mountaineering safety. Actual independent units,calibration,measurement definitions/coverage and model applicability;not a climate forecast,causal determination,geodesy operation or safe travel/design approval.
Description
A restricted dry-crevasse model balances uniform tensile stress against overburden to estimate penetration depth.
A restricted dry-crevasse model balances uniform tensile stress against overburden to estimate penetration depth.1
Water pressure, changing stress and fracture mechanics are outside its assumptions.
When to use Crevasse Penetration Tensile Stress Calculator
Use this tool to apply the stated crevasse penetration tensile stress calculator operation with an explicit input and unit basis.
How to use Crevasse Penetration Tensile Stress Calculator and how it works
- Establish the measurement basis and units described above.
- Enter callerIndependentDepthUniformTensileStress, actualIceDensity, callerGravity and run the tool.
- Read result.value using the output meanings below.
- If input is rejected, correct the stated type, range, ordering or alignment issue and rerun; review successful results under the declared convention.
| Input field | Meaning | Value type | Requirement |
|---|---|---|---|
| callerIndependentDepthUniformTensileStress | Depth uniform tensile stress, on the basis specified in the algorithm. | number | required; finite; nonnegative; further conditions in the algorithm |
| actualIceDensity | Ice density, on the basis specified in the algorithm. | number | required; finite; strictly positive; further conditions in the algorithm |
| callerGravity | Gravity, on the basis specified in the algorithm. | number | required; finite; strictly positive; further conditions in the algorithm |
Require nonnegative tensile stress and positive ice density and gravity. Return twice stress divided by density times gravity; coherent SI inputs produce meters.
depth = 2 × tensile stress / (ρice g) Apply the declared units, ordering and branch conditions.
| Output field | Meaning | Value type |
|---|---|---|
| result | Object containing the declared output fields. | object |
| result.value | Restricted dry-crevasse depth in meters with coherent SI inputs. | number |
{
"input": {
"callerIndependentDepthUniformTensileStress": 1,
"actualIceDensity": 1,
"callerGravity": 1
},
"output": {
"result": {
"value": 2
}
}
}Limitations and assumptions
The output applies the declared operation to the values you supply. Establish the measurement basis, units, coefficients and any caller-selected rules before interpreting it. The tool does not independently collect or verify observations or decide whether a model or reference applies. The simplified geometry or force calculation does not establish structural capacity, flotation stability or safe travel conditions.
Supply explicit required fields with the documented types and dense aligned arrays. Unknown fields, wrong types and nonfinite numbers are rejected. Branch-specific constraints are explained above. A successful false boolean, negative signed difference, empty slice or unresolved tie is distinct from an input error. Very large inputs or outputs may be rejected by shared resource limits.
Alternative or Complementary methods
For a related operation, use Driving Stress Calculator. A local slab driving-stress model combines ice density, gravity, thickness, slope and a shape factor.
For a related operation, use Degree Day Factor Melt Water Equivalent Calculator. A degree-day melt model scales positive temperature accumulation by a calibrated water-equivalent melt factor.
References
Similar or alternative tools
- Driving Stress Calculator
A local slab driving-stress model combines ice density, gravity, thickness, slope and a shape factor.
- Degree Day Factor Melt Water Equivalent Calculator
A degree-day melt model scales positive temperature accumulation by a calibrated water-equivalent melt factor.