Vertical wind tunnel experiments and a theoretical study on the microphysics of melting low-density graupel

It was found that mass and heat transfer in the dry stage is 2 times as high as that of liquid drops at the same Reynolds number. Based on the experimental results, a model was developed from which the external and internal convective enhancement factors during melting due to surface irregularities and internal motions inside the meltwater were derived using a Monte Carlo approach. The modeled total melting times and distances deviated by 10% from the experimental results.

Sensitivity tests with the developed model revealed strong dependencies of the melting process on relative humidity, lapse rate, initial graupel density, and graupel size. In dependence on these parameters, the total melting distance varied between 600 and 1200 m for typical conditions of a falling graupel.