/kənˈdɪʃənəlli: ʌnˈsteɪ.bəl/
noun
1. An atmospheric condition that exists when the environmental lapse rate is less than the dry adiabatic rate, but greater than the moist adiabatic rate. Also called conditional instability.
My life is basically a metaphor of a confused air parcel whose condition depends on the environment, a college environment that is constantly changing because I am totally insane sane.
