1. Dense fogs start to dissipate as the sun warms the saturated air . 2. Saturated air cools about three degrees for each 1, 000 feet of ascent.3. Water vapor in saturated air is normally attracted to circulation of the air. 4. When saturated air cools, it can no longer contain the same amount of water vapor. 5. For every 20 degrees the temperature falls, saturated air can have only half as much moisture. 6. A mild, moist flow from the northwest will add further moisture to the already saturated air . 7. An intense disturbance from the Pacific added extra lift to the seldomly saturated air on Sunday. 8. For every 20 degrees that the temperature falls, saturated air can have only half as much moisture. 9. Situations in which the equivalent potential temperature decreases with height, indicating instability in saturated air , are quite common. 10. Situations in which the equivalent potential temperature decreases with height, indicating instability in saturated air , are much more common.
