Why might dew form in the morning?(1 point)
Responses
The temperature fell overnight, and colder air can hold more water vapor.
The temperature fell overnight, and colder air can hold more water vapor.
The temperature rose overnight, and warmer air can hold less water vapor.
The temperature rose overnight, and warmer air can hold less water vapor.
The temperature fell overnight, and colder air can hold less water vapor.
The temperature fell overnight, and colder air can hold less water vapor.
The temperature rose overnight, and warmer air can hold more water vapo
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what
Sorry for the incomplete response. Dew forms in the morning when the temperature falls overnight, causing the air to cool down. Cooler air has a lower capacity to hold water vapor, so any excess moisture in the air condenses and forms dew on surfaces.
Why might dew form in the morning?(1 point)
Responses
The temperature fell overnight, and colder air can hold more water vapor.
The temperature fell overnight, and colder air can hold more water vapor.
The temperature rose overnight, and warmer air can hold less water vapor.
The temperature rose overnight, and warmer air can hold less water vapor.
The temperature fell overnight, and colder air can hold less water vapor.
The temperature fell overnight, and colder air can hold less water vapor.
The temperature rose overnight, and warmer air can hold more water vapo
r.
The temperature fell overnight, and colder air can hold more water vapor.
The temperature fell overnight, and colder air can hold more water vapor.
The correct answer is: The temperature fell overnight, and colder air can hold more water vapor.
Explanation:
Dew forms in the morning when the temperature of the air drops overnight. When the temperature drops, the air becomes cooler, and cooler air can hold less moisture or water vapor. As a result, the excess moisture in the air begins to condense and form small water droplets on surfaces like grass, leaves, or car windshields, creating dew. This is because the air reaches its saturation point, where it can no longer hold all the water vapor, and the excess moisture condenses into liquid form.