Delta O18 Paleotemperature Calculator
Apply explicit caller local delta-18O reference/slope paleotemperature calibration; no universal isotope thermometer, age inference or correction for source/season/elevation changes.
Description
An isotope paleotemperature estimate depends on site-specific reference and slope.
An isotope paleotemperature estimate depends on site-specific reference and slope. Source, season and elevation can alter the relationship.1
Enter finite isotope/reference/temperature values and finite nonzero per-mille/°C slope. Return anomaly and calibrated °C; signed slopes are allowed.
When to use Delta O18 Paleotemperature Calculator
Use Delta O18 Paleotemperature Calculator when you need to evaluate the supplied records under the calculation and evidence rules below. No universal isotope thermometer, age or environmental-confound correction is supplied.
Prepare the observed ice, snow, water or geometry measurements and explicit calibration parameters requested. Keep coordinates, datum, density and time units consistent.
How to use Delta O18 Paleotemperature Calculator and understand its results
- Prepare the observed ice, snow, water or geometry measurements and explicit calibration parameters requested. Keep coordinates, datum, density and time units consistent.
- Enter deltaO18Permil, referenceDeltaO18Permil, referenceTemperatureC, callerCalibrationPermilPerC using the field table and calculation rules, then run the tool.
- Read calibratedPaleotemperatureC, isotopeTemperatureAnomalyC. The explanation below defines the units, signs, ordering and any flags or placeholder values.
- If the tool reports an input issue, correct the values and run it again. Apply the stated assumptions when interpreting a successfully returned result.
| Input field | Meaning | Value type; see rules below | Requirement |
|---|---|---|---|
| deltaO18Permil | Delta o18 permil | number | Required |
| referenceDeltaO18Permil | Reference delta o18 permil | number | Required |
| referenceTemperatureC | Reference temperature c | number | Required |
| callerCalibrationPermilPerC | Caller calibration permil per c | number | Required |
Enter finite isotope/reference/temperature values and finite nonzero per-mille/°C slope. Return anomaly and calibrated °C; signed slopes are allowed.
anomaly=(observedδ18O−referenceδ18O)/slope; temperature=referenceT+anomaly Units, indexing, boundary conditions and exceptional cases are defined in the calculation rules above.
| Output field | Meaning | Value type |
|---|---|---|
| calibratedPaleotemperatureC | Calibrated paleotemperature c | number |
| isotopeTemperatureAnomalyC | Isotope temperature anomaly c | number |
{
"input": {
"deltaO18Permil": -30,
"referenceDeltaO18Permil": -35,
"referenceTemperatureC": -20,
"callerCalibrationPermilPerC": 0.5
},
"output": {
"calibratedPaleotemperatureC": -10,
"isotopeTemperatureAnomalyC": 10
}
} Limitations and assumptions
No universal isotope thermometer, age or environmental-confound correction is supplied.
Numeric inputs, where present, must be finite. Follow the calculation-specific rules for overflow, underflow and exceptional cases. Missing required fields, extra fields, wrong value types and violations of the calculation rules are input errors.
Alternative or Complementary methods
Use Rate Factor Arrhenius Temperature Calculator: A single-regime Arrhenius model scales a reference ice rate factor with temperature. Regime and pressure applicability are external assumptions. For a complementary task, use Close Off Age Lock In Depth Calculator: Layer mass and steady accumulation can estimate ice residence age at supplied firn depths. Ice age differs from trapped-gas age.
References
-
Delta O18 Paleotemperature Calculator — tool.io
Similar or alternative tools
- Rate Factor Arrhenius Temperature Calculator
A single-regime Arrhenius model scales a reference ice rate factor with temperature. Regime and pressure applicability are external assumptions.
- Close Off Age Lock In Depth Calculator
Layer mass and steady accumulation can estimate ice residence age at supplied firn depths. Ice age differs from trapped-gas age.