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