Introduction : this calculator is used to demonstrate how one might use a mathematical model to "forecast" a meteorological variable, in this case a temperature dewpoint. In this calculator, it is assumed that one can measure (using simple meteorological measuring devices such as might be found at any home improvement store) two values:
Given these two values, how might one "forecast" a temperature dewpoint? A series of algorithms, or calculations, can be performed to determine the vapor pressure of water (in millibars, or mb) if the atmosphere is saturated (i.e, if the relative humidity is 100%) or the actual vapor pressure if the atmosphere is not completely saturated. The main equation is:
Once we have calculated the SVP, we can adjust it for an atmosphere that is less than completely saturated:
For example, in the calculator below, the input values are 10.0o Celsius with a relative humidity of 65%. The vapor pressure of a saturated atmosphere at the given temperature calculates (click on the "Evaluate" button) to 12.283 mb of pressure. What is the actual vapor pressure, given that the atmosphere is only at 65% of its capacity? The calculator provides a value of 7.984 mb of pressure. Once we have this value, we can forecast the current temperature dewpoint in degrees Celsius. Using the lookup table below the calculator, we need to determine the temperature which corresponds the closest to the actual vapor pressure, in this case a vapor pressure of 7.984 mb. Looking at the table, 7.984 mb is somewhere between 7.580 (a temperature of 3o Celsius) and 8.135 (a temperature of 4o Celsius).
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