When the air near the ground has enough moisture and the temperature reaches the dew point, condensation occurs, leading to the formation of dew, fog, or clouds. This process happens because the air can no longer hold all the moisture in the form of vapor, causing water droplets to form on surfaces or in the atmosphere. Dew is commonly seen on grass and other surfaces in the early morning, while fog can reduce visibility in the air. Overall, reaching the dew point signifies a transition from vapor to liquid in the atmosphere.
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