| 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.
|
