| MadSci Network: Earth Sciences |
The 'stability of air parcels' refers to whether or not they are prone to continued rising or sinking, when perturbed slightly. This is an important concept for the generation of clouds, and in general for considerations of transport (movement) of air, water vapor and other gases, vertically. A parcel of air may be unstable because lifting it slightly may make it even more buoyant in which case it will continue to rise. Unstable air may alternatively be able to continue sinking if displaced down slightly. Stable air behaves oppositely: it falls back if pushed up and bobs up if pushed down. Whether a parcel of air is stable or unstable has to do with thermodynamics and such things as the temperature and humidity of the parcel compared to the surrounding air - so it is a relative property of air parcels. Air may rise because it is unstable but then reach air where it no longer is unstable, and stop there. The theormodynamic properties of air changes as it is exposed to varying levels of pressure - think of how hot a bicycle pump becomes when you are using it: You are compressing the air inside and this makes the air hot. Air that is compressed and allowed to escape - such as air from a steel compressed air bottle, or air from a tyre - cools. Well, the same thing happens in Nature - if a parcel of air rises it will expand and thus cool, and this change of thermodynamic state could now alter its stability.
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