Strain Heating Contribution
Contract full symmetric stress and strain-rate tensors, counting off-diagonal shear twice; negative power is preserved and flagged as inconsistent with positive dissipation, not relabeled heating.
Description
Strain power contracts stress with deformation rate.
Strain power contracts stress with deformation rate. For symmetric tensors, off-diagonal shear components occur twice in the full contraction.1
Contract full symmetric stress and strain-rate tensors, counting off-diagonal shear twice; negative power is preserved and flagged as inconsistent with positive dissipation, not relabeled heating.
When to use Strain Heating Contribution
Use this for the following task: Contract full symmetric stress and strain-rate tensors, counting off-diagonal shear twice; negative power is preserved and flagged as inconsistent with positive dissipation, not relabeled heating.
Prepare the measurements and calibration parameters in the declared units. Keep vector entries aligned and choose a consistent spatial frame and time basis.
How to use Strain Heating Contribution and understand its results
- Prepare the measurements and calibration parameters in the declared units. Keep vector entries aligned and choose a consistent spatial frame and time basis.
- Enter stressTensorPa, strainRateTensorPerYear, secondsPerYear using the field table, then run the tool.
- Read signedVolumetricStrainPowerWattsPerM3, nonnegativeDissipationScreen. Interpret flags, units, ordering and placeholder values using the rules below.
- Review any reported issue or failed check, correct the supplied values when appropriate, and verify the result in its intended context.
| Input field | Meaning | Value type and bounds | Requirement |
|---|---|---|---|
| stressTensorPa | Stress tensor pa | list of list of number; each entry: list of number; each entry: number | Required |
| strainRateTensorPerYear | Strain rate tensor per year | list of list of number; each entry: list of number; each entry: number | Required |
| secondsPerYear | Seconds per year | number | Required |
Supply two exactly symmetric 3×3 tensors using tensor shear rates per year. Multiply corresponding components and sum; preserve negative power and report whether it is nonnegative.2
power_W/m³ = ΣiΣj σij ε̇ij / secondsPerYear This summarizes the declared operation. Units, indexing, inclusivity and exceptional cases are explained in the surrounding text.
| Output field | Meaning | Value type |
|---|---|---|
| signedVolumetricStrainPowerWattsPerM3 | Signed volumetric strain power watts per m3 | number |
| nonnegativeDissipationScreen | Nonnegative dissipation screen | boolean |
{
"input": {
"stressTensorPa": [
[
2,
1,
0
],
[
1,
3,
0
],
[
0,
0,
4
]
],
"strainRateTensorPerYear": [
[
1,
2,
0
],
[
2,
1,
0
],
[
0,
0,
-2
]
],
"secondsPerYear": 10
},
"output": {
"signedVolumetricStrainPowerWattsPerM3": 0.1,
"nonnegativeDissipationScreen": true
}
} Limitations and assumptions
Engineering shear rates differ by a factor of two. A negative result is not relabeled as heating and can indicate inconsistent supplied components.
Constants and empirical coefficients are supplied rather than calibrated. Check units and observational applicability before interpreting the model. Malformed requests produce input errors. A successfully evaluated request can still contain false flags, empty result lists or a result outside the supplied threshold; those outcomes have the meanings stated above.
Alternative or Complementary methods
Choose Glen Flow Law Strain Rate for this operation: Evaluate signed scalar Glen shear strain rate A·E·sign(tau)|tau|^n; A units follow n, and shear tensor strain rate differs by a factor two from engineering shear rate. For a complementary task, use Friction Heating Melt Contribution for this operation: Balance basal traction×sliding power and caller heat partition to ice melt at pressure melting; not geothermal heating or a sliding-speed prediction.
Further background: Ice rheology.
References
-
Ice rheology — PISM
-
Strain Heating Contribution — tool.io
Similar or alternative tools
- Glen Flow Law Strain Rate
Evaluate signed scalar Glen shear strain rate A·E·sign(tau)|tau|^n; A units follow n, and shear tensor strain rate differs by a factor two from engineering shear rate.
- Friction Heating Melt Contribution
Balance basal traction×sliding power and caller heat partition to ice melt at pressure melting; not geothermal heating or a sliding-speed prediction.