What happens when the rate of evaporation equals the rate of condensat...
Evaporation and Condensation
Evaporation is the process by which a liquid turns into a gas or vapor. On the other hand, condensation is the process by which a gas or vapor turns into a liquid. These two processes are essential in the water cycle.
Equilibrium between Evaporation and Condensation
When the rate of evaporation equals the rate of condensation, it means that the liquid has reached a state of equilibrium. At this point, the amount of water vapor being released into the air is equal to the amount of water vapor that is being condensed into liquid.
Dew Point
The dew point refers to the temperature at which the air becomes saturated with water vapor. When the rate of evaporation equals the rate of condensation, the dew point is reached. This means that the air cannot hold any more water vapor, and any excess water vapor will start to condense into liquid.
Cloud Formation
When the rate of evaporation exceeds the rate of condensation, water vapor will continue to rise into the atmosphere. As the water vapor rises, it cools and condenses into tiny water droplets or ice crystals, forming clouds. Therefore, when the rate of evaporation equals the rate of condensation, clouds will not form.
Conclusion
In summary, when the rate of evaporation equals the rate of condensation, the dew point is reached, and no more water vapor can be held in the air. This means that there will be no cloud formation, and any excess water vapor will condense into liquid.
What happens when the rate of evaporation equals the rate of condensat...
When the rate of evaporation equals the rate of condensation:
- The dew point is reached (Answer C)
- The dew point is the temperature at which air becomes saturated with water vapor, meaning it cannot hold any more moisture.
- When the rate of evaporation (water vapor entering the air) equals the rate of condensation (water vapor leaving the air), the air is saturated and has reached its dew point.
- At this point, any further cooling of the air or addition of moisture will result in condensation, which can lead to the formation of dew, frost, or fog.
- The dew point is an important factor in determining the relative humidity and comfort levels in the atmosphere.
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