Description
Return snow-water-equivalent depth.
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 snow-water-equivalent depth.
When to use this tool
Use Snow Water Equivalent Density Term when checking the stated atmospheric pressure, temperature, humidity or water-basis term.
How to use the tool and how it works
- Enter snowDepth, snowDensity, waterDensity. Use the units and conventions below.
- Run the tool. Correct any format, range, or cross-field input error before interpreting the output.
- Read waterEquivalentDepth. Use the output convention below.
Return snow-water-equivalent depth. Require nonnegative snowDepth/snowDensity and waterDensity > 0; waterEquivalentDepth = snowDepth*snowDensity/waterDensity.1
| Input field | Meaning and units | Accepted input |
|---|---|---|
| snowDepth | Snow Depth | Required. Finite number; minimum 0. |
| snowDensity | Snow Density | Required. Finite number; minimum 0. |
| waterDensity | Water Density | Required. Finite number; strictly above 0. |
| Output field | Interpretation | Returned shape |
|---|---|---|
| waterEquivalentDepth | Water Equivalent Depth | Required. Finite number. |
{
"input": {
"snowDepth": 0.5,
"snowDensity": 200,
"waterDensity": 1000
},
"output": {
"waterEquivalentDepth": 0.1
}
}Limitations and assumptions
- Depth units carry through and densities need a common mass/volume basis; layering, actual density and snowpack hazards are not assessed.
- 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
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