12) The answer is that due to any such imbalance the normal equilibrium distribution of Kinetic Energy (KE) and Potential Energy (PE) is upset and
parcels of air start to move around differently relative to each other due to the changes in their respective KE and PE contents.
Not exact matches
Wikipedia
starts with «The dry adiabatic lapse rate (DALR) is the rate
of temperature decrease with height for a
parcel of dry or unsaturated
air rising under adiabatic conditions.»
«Take two identical volumes (
parcels)
of air, taken from somewhere at a midlevel in the troposphere, with each
parcel containing an identical number
of gas molecules and the same amount
of heat energy to
start.
Viscosity is to
air what friction is to a book sliding across a table — even if you
start the book with some velocity relative to a table (or a
parcel of air with some velocity relative to other
parcels) viscosity will quickly bring the motion to a halt.