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Equations are presented which relate saturation vapor pressure to temperature for moist air. The equations are designed to be easily implemented on a calculator or computer and can be used to convert in either direction. They are more accurate than the commonly used Goff-Gratch equations for the meteorologically interesting region of −80 to +50°C. Equations also are given for the enhancement factor.
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Arden L. Buck (Tue,) studied this question.
www.synapsesocial.com/papers/69c3b806f26b310bd10861d4 — DOI: https://doi.org/10.1175/1520-0450(1981)020<1527:nefcvp>2.0.co;2
Arden L. Buck
Journal of applied meteorology
NSF National Center for Atmospheric Research
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