Condensation

Condensation is the process by which water vapor, a gaseous form of water, turns into liquid water. This occurs when the temperature of the air drops and it can no longer hold all of the water vapor it contains. As a result, the excess water vapor condenses into tiny liquid water droplets, forming clouds, fog, or dew.

Factors Affecting Condensation

• Temperature: Lowering the temperature of the air increases the likelihood of condensation.
• Humidity: Higher humidity levels mean there is more water vapor in the air, increasing the potential for condensation.
• Surface: Condensation can occur on surfaces that are cooler than the surrounding air, such as the surface of a cold drink or a bathroom mirror after a hot shower.

Examples of Condensation

Condensation can be observed in various everyday scenarios:

• Formation of dew on grass in the morning
• Steam turning into water droplets on a bathroom mirror
• Cloud formation in the sky
• Water droplets forming on the outside of a cold glass

Study Guide

When studying condensation, it's important to understand the key concepts and factors that influence this process. Here are some key points to focus on:

1. Define condensation and explain how it occurs.
2. Discuss the role of temperature and humidity in condensation.
3. Identify and describe everyday examples of condensation.
4. Explain the significance of condensation in the water cycle.

Additionally, conducting hands-on experiments or observations related to condensation can help reinforce the understanding of this concept.

Remember to review the material regularly and practice applying the concepts to different scenarios to solidify your understanding of condensation.