How is Dew made?

Dew is formed when water vapor in the air condenses into liquid water droplets on cool surfaces. This process occurs when the air near the ground is cooler than the air above it, causing the water vapor to condense. Dew is most common in the early morning, when the air is coolest, and on clear nights, when there is less heat to keep the ground warm.

The process of dew formation can be explained using the following steps:

1. Evaporation: During the day, the sun heats the ground, causing water to evaporate from the soil and plants.

2. Condensation: At night, the ground cools down, causing the water vapor in the air to condense into tiny water droplets. This process is similar to how clouds form in the sky.

3. Deposition: The water droplets then settle on cool surfaces, such as grass, leaves, and car windows.

Dew is an important source of moisture for plants, especially in dry climates. It also helps to cool the air and provides a habitat for small insects and animals.