Figure 3.16
Adiabatic temperature change. As air parcels move vertically in the atmosphere, they cool or warm because of changes in their volume. This unsaturated parcel is cooling and warming at the dry adiabatic rate of 10°C per 1,000 m.Figure 3.16
Adiabatic temperature change. As air parcels move vertically in the atmosphere, they cool or warm because of changes in their volume. This unsaturated parcel is cooling and warming at the dry adiabatic rate of 10°C per 1,000 m.