Heat. Hot air holds more vapor than cold air. This is why we get rain when hot air rises, cools down, and the water vapor condenses out to form rain drops. It's also why we get clouds, the vapor condenses when the air gets cold at altitude but not enough to form droplets and fall from the sky.
condenses- loses heat and thus becomes a solid
The higher the temperature of the air the higher the amount of humidity you feel. Also the colder the airs temperature it can cause precipitation such as hail, snow, and sleet rather then just rain.
Tornadoes generally do not form over large bodies water and usually only cross lakes, ponds and rivers. Their brute strength is equally powerful over land and these small bodies of water. Tornadoes have been known to dry lakes on occasion and cause fish to rain on people's houses in rare instances.
n.A headlong fall or rush.Abrupt or impulsive haste.A hastening or acceleration, especially one that is sudden or unexpected: He is responsible for the precipitation of his own demise.Meteorology. Any form of water, such as rain, snow, sleet, or hail, that falls to the earth's surface.The quantity of such water falling in a specific area within a specific period.Chemistry. The process of separating a substance from a solution as a solid.the answer is within the question then in the answer sh duhhhhhhhhhhhh
The duration of sex odor can vary depending on individual factors such as hygiene, diet, and overall health. However, proper hygiene practices such as showering before and after sex, changing clothes, and using unscented products can help to reduce and eliminate any lingering odors.
Air's ability to hold water vapor increases as temperature increases. Warmer air can hold more water vapor compared to cooler air.
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 air gets warmer, it's ability to hold water vapor increases.
Temperature is the main variant of air's ability to hold moisture. The warmer the air the more water it can hold without condensation.
As the temperature of the air increases, water gets evaporated and hence the water content (humidity) decreases. As temperature reduces the temperature of the water vapour also reduces and it cannot maintain it's gaseous form so undergoes a phase transition to a liquid, or even straight to ice, which happens more readily at cold surfaces ('frost). The temperature is called the 'dew point'. At a microscopic level the process is rather more complex than that, quite interesting and counter intuitive.
The ratio of air's water vapor content to its capacity to hold water vapor at the same temperature is known as the relative humidity. It is expressed as a percentage and indicates how close the air is to being fully saturated with water vapor at that temperature. A relative humidity of 100% means the air is holding the maximum amount of water vapor it can at that temperature.
Air can hold a certain amount of water vapour. The amount it can hold depends on the air temperature - the hotter it is, the more water it can hold. A way to think of it is that water Can dissolve in air, just like some gases and solids can dissolve in water.
When temperature increases, air can hold more water vapor because warm air molecules are further apart, creating space for more water molecules to be held. Conversely, when temperature decreases, air can hold less water vapor because cool air molecules are closer together, leaving less space for water molecules.
This is called the Airs "Relative" humidity. The more water vapor in the atmosphere the higher the relative humidity will be.
condenses- loses heat and thus becomes a solid
because they float and airs lighter because they float and airs lighter