31. Condensation releases latent heat which must be dissipated in order for water collection to continue. 32. Convection and release of latent heat transports energy from the surface into the upper atmosphere. 33. When the water evaporates, it cools the air by converting sensible heat to latent heat . 34. The release of latent heat is an important source of energy in the development of thunderstorms. 35. Both sensible and latent heats are observed in many processes of transport of energy in nature. 36. The loss of heat through conduction is reduced when water freezes, and latent heat is released. 37. Such usage referred to " latent heat of expansion " and several other related latent heats. 38. The calculated latent heat of vaporization values for the investigated 45 elements agrees well with experiments. 39. The phase changes release latent heat , heating the cloud and driving it to yet higher altitudes. 40. Such usage referred to " latent heat of expansion " and several other related latent heats .
