e/Convective overshoot

Information
has gloss	eng: Convective overshoot is a phenomenon of convection carrying material beyond an unstable region of the atmosphere into a stratified, stable region. Overshoot is caused by the momentum of the convecting material, which carries the material beyond the unstable region.
lexicalization	eng: Convective overshoot
instance of	(noun) a visible mass of water or ice particles suspended at a considerable altitude cloud