I probably should add that melting is a latent cooling process too. If you think of the stages of water as having increasing energy from solid to liquid to gas, anytime you go up a phase change to a higher energy state it requires taking the energy from the environment. So the snow needs heat energy to complete the phase change from solid to liquid. It takes that thermal energy from the air around it. Up in a cloud, if you have condensation (gas to a liquid droplet) or deposition (gas directly to an ice crystal) the H2O is "losing" heat to the environment. We talk about latent heating a lot with convection and hurricanes because of the massive amounts of condensation being produced by those types of systems.
Deposition, Condensation, Freezing >>> Latent heating of the air
Sublimation, Evaporation, Melting >>> Latent cooling of the air
So in the case of a day like today, we have temps near 40F in much of NH with RH near 15%. So we're getting a little of all 3 latent cooling processes. IOW, not much loss in the heart of the pack, but probably a decent amount lost along exposed edges.