Clouds & diabatie and adiabatic processes let's imagine we have an air parcel at the surface whose temperature is 25°c and whose dew point temperature is 20°c. if this parcel were to rise from the surface, would it cool at the dry adiabatic lapse rate or the moist adiabatic lapse rate and why? (2 pts.) 2) the parcel is now lifting and cooling at the correct lapse rate. if the air parcel is unsaturated does the lcl represent in terms of air parcel humidity, and why is it important for cloud formation? (5 pts.) when it begins its ascent, it may rise all the way to its lifting condensation level (lcl). what 3) once our air parcel reaches the lcl will it cool at the dry adiabatic lapse rate or moist adiabatic lapse rate and why? (2 pts.)