hurrycan
Water vapour is a constituents in air because water vapour rises in the atmosphere & is always present in the atmospere in some or the other quantity.Also 0.0001% of air consist water vapour
When the water vapour condenses and turns into a liquid.
As air rises it becomes decompressed, which causes it to cool. This cooling can cause water vapor to condense, forming clouds.
Water Vapour is considered as gas and since its particles are spread out it is light and therefore able to rise up into the clouds. As the clouds gather/collect water vapour it gets heavier. Cold air cools down the water vapour turning it back into water droplets and fall back to the ground.
Water vapor rises upwards because it is less dense than the surrounding air. When water evaporates, it turns into gas, which occupies more space than its liquid form, causing it to become lighter. Additionally, as warm air rises, it carries the water vapor with it, contributing to the process of convection in the atmosphere. This upward movement is essential for cloud formation and precipitation.
The water vapour rises to form clouds.
it becomes water vapour in the air
When water heats up, it rises as vapor and as temperature drops at high altitudes, the vapor condenses and becomes clouds. With time, the condensed water soon liquidifies and becomes rain.
Water vapour is a constituents in air because water vapour rises in the atmosphere & is always present in the atmospere in some or the other quantity.Also 0.0001% of air consist water vapour
hurrycan
When the water vapour condenses and turns into a liquid.
by evaporation
the humidity condences and you get pure water. the air can only hold a certain amount of water vapour, that amount rises with temp so when you cool the air you can have excess water vapour which will condence to liquid water.
It cools and consequently can hold less water vapour. The vapour condenses and it rains. This is convection rainfall.
It cools and consequently can hold less water vapour. The vapour condenses and it rains. This is convection rainfall.
Condensation in the water cycle is the process where water vapor in the air cools and turns back into liquid water, forming clouds. This occurs when warm air rises, cools, and reaches its dew point, causing the water vapor to condense into water droplets. These water droplets eventually coalesce into clouds and can further develop into precipitation.
The air that you exhale contains water vapour. When you exhale during a cold day, the relative humidity increases. Relative humidity is actually the percentage of the amount of water vapour in the air.(the maximum amount of water vapour that the air can hold at that temperature) The colder the air, the less water vapour it can carry. When exhaled, air mixes with cold air, the temperature of the exhaled air drops, but there is more water vapour. When the air becomes saturated, (relative humidity is 100%), the extra water vapour will condense, allowing you to see your breathe on cold days.