Warm air can hold more water vapor.
warmer as it condenses and releases energy to the ground. This can lead to the formation of fog.
When condensation releases heat, it warms the surrounding air. The warming air can indirectly affect the temperature of the land below by creating temperature inversions or modifying weather patterns.
As warm air rises, it expands and becomes less dense. This causes it to cool down, leading to the formation of clouds and potentially precipitation. The movement of warm air rising is part of the process known as convection.
At increased temperatures, atoms and molecules exhibit more kinetic energy. This energy shows up as "vibration" in the atom or molecule. Those atoms and molecules also move around more in the "situation" they're in. As a liquid or gas, those particles that make it up will move around more within the volume of that liquid or gas. In a solid, the atoms or molecules will "buzz" increasingly as temperature goes up.
to form
it evaporates
it gets warmer
it gets warmer
it gets warmer
As the air gets warmer, it's ability to hold water vapor increases.
it gets warmer as it rises
It causes the air to be dry, and it gets warmer.
As the air gets warmer, it's ability to hold water vapor increases.
As the air gets warmer, it's ability to hold water vapor increases.
As the day gets warmer, dew evaporates into the air. The sun's heat causes water droplets to turn from a liquid state into water vapor, which then rises into the atmosphere.
it gets warmer then it gets colder
As the air gets warmer, it's ability to hold water vapor increases.