It forms clouds.
Further condensation creates rain hail .
The transition from atmosphere to clouds occurs when water vapor in the air cools and condenses into tiny water droplets or ice crystals. This process typically happens when warm, moist air rises and expands, leading to cooling. As the air cools to its dew point, the water vapor condenses around particles like dust or pollen, forming visible clouds. Thus, clouds represent a collection of these condensed water droplets or ice crystals suspended in the atmosphere.
Clouds form when water vapor in the atmosphere cools to its dew point and then condenses into tiny water droplets or ice crystals. This process occurs when the air becomes saturated and can no longer hold all the water vapor, leading to the formation of visible clouds. The condensation typically happens around small particles in the atmosphere, such as dust or pollen, which act as nuclei for the droplets. As more water vapor condenses, the clouds become thicker and more prominent.
When water vapor rises high in the atmosphere and cools, it condenses into tiny water droplets or ice crystals. This can happen because the air at higher altitudes is colder, causing the water vapor to reach its dew point temperature and change from a gas to a liquid or solid form.
Water vapor in the water cycle evaporates from bodies of water, rises into the atmosphere, cools and condenses to form clouds, and then falls back to the Earth's surface as precipitation in the form of rain, snow, sleet, or hail. This cycle of evaporation, condensation, and precipitation repeats continuously.
Water vapor condenses into liquid water primarily in the atmosphere, particularly when it cools to its dew point. This process often occurs in clouds, where rising air cools and the water vapor condenses into tiny droplets. Additionally, condensation can happen on surfaces when warm, moist air comes into contact with cooler surfaces, leading to phenomena like dew or fog.
It condenses into liquid.
When water vapor cools and condenses into a cloud, this process is called condensation. This happens when the water vapor reaches its dew point temperature and changes back into liquid water droplets, which then cluster together to form clouds in the atmosphere.
Before water condenses in clouds, warm air rises and cools as it ascends higher into the atmosphere. As the air cools, it reaches its dew point temperature, causing water vapor to condense into tiny water droplets or ice crystals. These droplets then come together to form clouds.
When water vapor cools and condenses into water droplets, it forms clouds in the atmosphere. This process is crucial for cloud formation, as the water droplets accumulate and interact with other particles in the air to create visible cloud structures.
I don't think you can condense a liquid, you can evaporate a liquid eg water which turnns into water vapour then when the water vapour gets colder it cools and condenses
The transition from atmosphere to clouds occurs when water vapor in the air cools and condenses into tiny water droplets or ice crystals. This process typically happens when warm, moist air rises and expands, leading to cooling. As the air cools to its dew point, the water vapor condenses around particles like dust or pollen, forming visible clouds. Thus, clouds represent a collection of these condensed water droplets or ice crystals suspended in the atmosphere.
A dew point is the amount of moisture in the air so as the air cools water condenses and form clouds.
When water vapor condenses around dust particles a cloud is formed
it condenses on the ground to make dew
After water evaporates, it turns into water vapor and rises into the atmosphere. Once in the atmosphere, the water vapor cools and condenses to form clouds. Subsequently, the water falls back to the Earth's surface as precipitation.
Clouds form when water vapor in the atmosphere cools to its dew point and then condenses into tiny water droplets or ice crystals. This process occurs when the air becomes saturated and can no longer hold all the water vapor, leading to the formation of visible clouds. The condensation typically happens around small particles in the atmosphere, such as dust or pollen, which act as nuclei for the droplets. As more water vapor condenses, the clouds become thicker and more prominent.
Water condenses in the atmosphere when warm air rises and cools, causing the water vapor in the air to change into liquid droplets. This process is known as condensation.