1. Explain how dew, frozen dew, and frost are visible.
2. Vary between cold fog, humid wet, and fog.
3. When the relative humidity of the air is less than 100 percent, can it form fog?
4. Name and description of four types of fog.
5. Why do winter fogs usually "burn off" in the late afternoon?
6. As many positive consequences of fog as you can.
7. List and describe the three methods of fog dispersion?
8. How is a radiation element normally formed?
9. Are the atmospheric conditions necessary for the development of fog mixture?
10. How does evaporation (mixing) fog form?
11. Clouds are more generally classified from the height above the ground, the surface is a list of large values of height and cloud types
List associated with each
12. List at least two recognizable features from each of the ten lower clouds
13. Why are clouds usually thin? Why are they almost entirely composed of ice crystals?
14. How can you tell Altostratus from cirrostratus?
Dew, frozen dew, and frost are all related to the presence of moisture in the atmosphere and the cooling of surfaces. Let's explore how each of them becomes visible:
In summary, dew, frozen dew, and frost are all visible due to the condensation or direct transition of water vapor into liquid droplets (dew) or solid ice crystals (frozen dew and frost) on surfaces when the temperature drops below the dew point or freezing point, respectively. These phenomena occur in specific weather conditions and add to the beauty of the natural world, often providing captivating views early in the morning.
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