Midchapter summary The air temperature in a rising parcel of unsaturated air decreases at the dry adiabatic rate, while the air temperature in a rising parcel of saturated air decreases at the moist adiabatic rate. The dry adiabatic rate and moist adiabatic rate of cooling are different due to the fact that latent heat is released in a rising parcel of saturated air. In a stable atmosphere, a lifted parcel of air will be cooler (heavier) than the air surrounding it, and will tend to sink back to its original position. In an unstable atmosphere, a lifted parcel of air will be warmer (lighter) than the air surrounding it, and will continue to rise upward, away from its original position. The atmosphere becomes more stable (stabilizes) as the surface air cools and/or the air aloft warms. The atmosphere becomes more unstable (destabilizes) as the surface air warms and/or the air aloft cools. Layered clouds tend to form in a stable atmosphere, while cumuliform clouds form in an unstable atmosphere.
Sample test questions If the environmental lapse rate is 5 deg C per 1000 m and the temperature at the earth's surface is 25 deg C, then the air temperature at 2000 m above the ground is: ♦ a.25 deg C ♦ b.35 deg C ♦ c.20 deg C ♦ d.15 deg C ♦ e.10 deg C
Sample test questions Take the dry adiabatic lapse rate to be 10 deg C per 1000 m. A radiosonde has measured the temperature of the atmosphere to be 30 deg C on the ground and 15 deg C at an altitude of 1000 m. What can you say about the stability of the atmosphere? ♦ The atmosphere is absolutely unstable ♦ The atmosphere is conditionally unstable ♦ The atmosphere is absolutely stable ♦ The atmosphere is neutrally stable ♦ This question cannot be answered without knowing the moist adiabatic lapse rate
How does the Stability of the Atmosphere Change During the Day? Daytime: ♦ The sun heats the ground. ♦ The boundary layer is heated from below. ♦ The environmental lapse rate is steep. ♦ The atmosphere can become unstable. Morning and evening hours: ♦ Radiation cooling results in temperature inversion. ♦ The boundary layer is cooler than the air above. ♦ The environmental lapse rate becomes less steep. ♦ The atmosphere is stable.
Air Stability Solar radiation The ground is warm IR cooling Altitude Temperature [C] Adiabatic lapse rate 3020 Environmental lapse rate The ground is cool DAY NIGHT