Geography · Ch 16 — Water in the Atmosphere
Dew
16.3.1
Dew
Dew forms when water vapour in the air condenses directly onto cooler solid surfaces — stones, grass blades, plant leaves — rather than onto dust or smoke particles floating in the air above the ground. The key distinction is the surface: the moisture settles on objects, not on nuclei suspended in the atmosphere.
The ideal conditions for dew formation are:
- Clear sky — allows the ground to cool rapidly by radiating heat away at night
- Calm air — still conditions keep the cooled air near the surface in contact with the objects, so condensation can occur
- High relative humidity — the air is already close to saturation, so only slight cooling is needed
- Cold and long nights — prolonged cooling brings the surface temperature down enough for condensation …
DefinitionDew
After condensation the water vapour or the moisture in the atmosphere takes one of the following forms -- dew, frost, fog and clouds. Forms of condensation can be classified on the basis of temperature and location. Condensation takes place when the dew point is lower than the freezing point as well as higher than the freezing point. …