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M. Issa Lélé and Peter J. Lamb

Weather Interactive Processing System (AWIPS) empirical algorithm for T d estimation (information online at http://meted.ucar.edu/awips/validate/dewpoint.htm ). This calculation involved several steps. First, the saturation vapor pressure ( e s ) corresponding to the Tmin was computed using an integrated form of the Clausius–Clapeyron equation. Second, the resulting e s was used with the RH max to obtain the corresponding vapor pressure ( e ). Finally, this e was employed in the calculation of

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