When vapor condenses into water droplets, it occurs when the temperature of the vapor decreases or when it comes into contact with a cooler surface, causing the molecules to lose energy. This process releases latent heat, which warms the surrounding air. As the vapor cools, it changes from a gaseous state to a liquid state, forming tiny droplets. This phenomenon is commonly observed in the formation of clouds, dew, and fog.
When you see a cloud, you are seeing water droplets, not water vapor. Clouds form when water vapor in the atmosphere cools and condenses into tiny liquid water droplets or ice crystals. These droplets cluster together, making the cloud visible. So, while the cloud originates from water vapor, what you see is actually the condensed water droplets.
Clouds form in the sky when water vapor condenses into water droplets. This process occurs when warm, moist air rises, cools, and reaches its dew point, causing the water vapor to condense and form visible clouds.
That describes a cloud.
Clouds form in the sky when water vapor condenses into water droplets. This process occurs when warm, moist air rises and cools, causing the water vapor to condense around particles in the atmosphere, such as dust or pollen, forming clouds.
Water vapor in the cool air condenses in to tiny droplets of water, forming clouds.
When water condenses, it changes from a gas (water vapor) to a liquid (water droplets). This process occurs when the temperature of the water vapor decreases, causing the molecules to come together and form liquid droplets.
It condenses out as droplets or ice crystals.
Water evaporates into water vapour, and water vapour condenses into water.
When cooled, water vapor condenses into tiny water droplets due to a decrease in temperature, leading to the formation of clouds or fog. This process occurs when the air becomes saturated with water vapor, causing it to change from a gas to a liquid state.
saturation point
fog
It is called fog. Fog is formed when water vapor condenses into tiny water droplets near the ground, reducing visibility.
That is the water vapor from our breath, that condenses to water droplets. Water vapor by itself is invisible - it becomes visible when it forms droplets.
When you see a cloud, you are seeing water droplets, not water vapor. Clouds form when water vapor in the atmosphere cools and condenses into tiny liquid water droplets or ice crystals. These droplets cluster together, making the cloud visible. So, while the cloud originates from water vapor, what you see is actually the condensed water droplets.
As the air cools, it can contain less and less water vapor as a gas. So the vapor condenses and creates visible mist called fog, clouds, drizzle, and rain depending on where the water vapor condenses and how much of it condenses. The rain and drizzle forms as the mist groups together and creates the droplets and drops.
They form through condensdation - that is, the water vapor in the air condenses.
Clouds form in the sky when water vapor condenses into water droplets. This process occurs when warm, moist air rises, cools, and reaches its dew point, causing the water vapor to condense and form visible clouds.