Unstable atmosphere (pg.52) - an unstable atmosphere can be noted by the ambient lapse
rate. We know that the standard lapse rate is about 2 degrees Celsius per 1000' of
altitude. If the ambient lapse rate is greater than the standard lapse rate (i.e. the
temperature is decreasing rapidly as you climb), this means the atmosphere is unstable.
Sufficient Moisture - the temperature/dew point spread can be used to determine how
moist the air is. The closer the temperature and dew point spread, the closer the air is to
becoming saturated or so full of moisture that it can hold no more. Warmer air can hold
more moisture than cooler air.
Lifting Action - Some of these lifting actions may include heating from below (rising
warm air called thermals), orographic lifting (wind pushing a moist unstable air mass
upslope), or frontal lifting (a fast moving cold front displacing warm, moist, and unstable
warmer air for example).