Compare and contrast the normal lapse rate, environmental lapse rate, the dry adiabatic rate, and the moist adiabatic rate
What will be an ideal response?
The normal lapse rate is the average decrease in temperature with increasing altitude, a value of 6.4 C°/1000 m (3.5 F°/1000 ft). However, the actual rate van vary greatly in space and time. The environmental lapse rate (ELR) is the actual lapse rate at a particular place at a particular time. The rate at which dry (i.e. not saturated) air cools by expansion as it rises, an average value of 10 C°/1000 m (5.5 F°/1000 ft). The moist adiatatic rate, the rate at which a saturated air parcel cools as it rises, has an average value of 6 C°/1000 m (3.3 F°/1000 ft). The se adiabatic rates also apply to the warming of descending air.
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