Description
Return dry-adiabatic temperature pressure scaling.
Atmospheric state formulas depend on absolute temperature, pressure reference, water mass/volume bases and layer assumptions. Local adiabatic, hydrostatic or precipitation terms can illustrate a supplied model without reconstructing an actual profile, validating an instrument or predicting weather hazards.
Return dry-adiabatic temperature pressure scaling.
When to use this tool
Use Dry Adiabatic Temperature Pressure Ratio when checking the stated atmospheric pressure, temperature, humidity or water-basis term.
How to use the tool and how it works
- Enter initialTemperature, initialPressure, finalPressure, exponent. Use the units and conventions below.
- Run the tool. Correct any format, range, or cross-field input error before interpreting the output.
- Read temperature. Use the output convention below.
Return dry-adiabatic temperature pressure scaling. Require initialTemperature and both pressures > 0; temperature = initialTemperature*(finalPressure/initialPressure)^exponent.1
| Input field | Meaning and units | Accepted input |
|---|---|---|
| initialTemperature | Initial Temperature | Required. Finite number; strictly above 0. |
| initialPressure | Initial Pressure | Required. Finite number; strictly above 0. |
| finalPressure | Final Pressure | Required. Finite number; strictly above 0. |
| exponent | Exponent | Required. Finite number. |
| Output field | Interpretation | Returned shape |
|---|---|---|
| temperature | Temperature | Required. Finite number. |
{
"input": {
"initialTemperature": 300,
"initialPressure": 100000,
"finalPressure": 50000,
"exponent": 0.25
},
"output": {
"temperature": 252.26892457611436
}
}Limitations and assumptions
- Temperature must be absolute and exponent is supplied; moisture, latent heat, irreversible mixing and actual parcel paths are omitted.
- Inputs must satisfy both the field types and the cross-field conditions above. Invalid input causes an error; a successful false flag or documented placeholder is a different result.
- Numeric calculations use binary floating point unless exact decimal-integer arithmetic is explicitly stated. No hidden measurement tolerance or decimal rounding is added; nonfinite or out-of-contract results are rejected. Numeric signed-zero results are exported as zero.
Alternative or Complementary methods
Use verified observations and an appropriate complete thermodynamic/profile analysis with explicit units, references and moisture assumptions for meteorological conclusions.
References
Similar or alternative tools
- Potential Temperature Pressure Sensitivity
Return pressure sensitivity of a potential-temperature term.
- Potential Temperature Reference Ratio
Return potential-temperature scaling with a supplied exponent.