Ice Core Layer Thinning Depth

Propagate layer thickness through supplied vertical-strain residence intervals; negative strain thins and positive strain thickens, without inferring strain from depth.

Description

Vertical strain changes the thickness of an annual ice layer as it travels through the ice column.

Vertical strain changes the thickness of an annual ice layer as it travels through the ice column. Negative strain thins a layer; positive strain thickens it.1

Propagate layer thickness through supplied vertical-strain residence intervals; negative strain thins and positive strain thickens, without inferring strain from depth.

When to use Ice Core Layer Thinning Depth

Use this for the following task: Propagate layer thickness through supplied vertical-strain residence intervals; negative strain thins and positive strain thickens, without inferring strain from depth.

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 Ice Core Layer Thinning Depth and understand its results

  1. Prepare the measurements and calibration parameters in the declared units. Keep vector entries aligned and choose a consistent spatial frame and time basis.
  2. Enter initialAnnualLayerThicknessM, residenceDurationsYears, verticalStrainRatesPerYear using the field table, then run the tool.
  3. Read cumulativeLogThinning, thinnedAnnualLayerThicknessM. Interpret flags, units, ordering and placeholder values using the rules below.
  4. Review any reported issue or failed check, correct the supplied values when appropriate, and verify the result in its intended context.
Input fieldMeaningValue type and boundsRequirement
initialAnnualLayerThicknessMInitial annual layer thickness mnumberRequired
residenceDurationsYearsResidence durations yearslist of number; each entry: numberRequired
verticalStrainRatesPerYearVertical strain rates per yearlist of number; each entry: numberRequired

Pair nonnegative residence durations with signed strain rates and multiply the positive initial layer thickness by the exponential cumulative factor.2

log factor = Σ ε̇vertical Δyears; thickness = initialThickness exp(log factor)

This summarizes the declared operation. Units, indexing, inclusivity and exceptional cases are explained in the surrounding text.

Output fieldMeaningValue type
cumulativeLogThinningCumulative log thinningnumber
thinnedAnnualLayerThicknessMThinned annual layer thickness mnumber
json
{
  "input": {
    "initialAnnualLayerThicknessM": 1,
    "residenceDurationsYears": [
      10,
      20
    ],
    "verticalStrainRatesPerYear": [
      -0.01,
      -0.02
    ]
  },
  "output": {
    "cumulativeLogThinning": -0.5,
    "thinnedAnnualLayerThicknessM": 0.6065306597126334
  }
}

Limitations and assumptions

Depth does not determine strain in this tool. The strain history must be supplied independently.

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 Annual Layer Count Age At Depth for this operation: Accumulate interpreted annual-layer counts and separately supplied hiatus years at depth boundaries; ambiguous/missing annuality must be resolved externally. For a complementary task, use Core Bottom Age Extrapolation for this operation: Integrate reciprocal exponentially thinning annual-layer thickness below a reference depth; explicitly a model extrapolation, not observed core chronology or an uncertainty bound.

Further background: Ice rheology.

References

  1. Ice rheology — PISM

  2. Ice Core Layer Thinning Depth — tool.io

Similar or alternative tools

  • Annual Layer Count Age At Depth

    Accumulate interpreted annual-layer counts and separately supplied hiatus years at depth boundaries; ambiguous/missing annuality must be resolved externally.

  • Core Bottom Age Extrapolation

    Integrate reciprocal exponentially thinning annual-layer thickness below a reference depth; explicitly a model extrapolation, not observed core chronology or an uncertainty bound.

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