Water vapor triggers convection currents that can form clouds.
When water boils, it turns into water vapor or steam. This water vapor rises into the air and eventually dissipates.
When water boils, bubbles form due to the release of water vapor from the liquid. These bubbles contain water vapor, not air. The water itself does not disappear; it is transformed into water vapor, which you see as bubbles.
The water goes in the air and forms into water vapor which turns into clouds.
Dry what? Perhaps the water is evaporated, and becomes vapor in the air.
Warmer air has higher saturation mixing ratios then cold air does. So therefore because of this 100% humidity in cold air is not 100% humidity in warmer air. The warmer the temperature, the more water vapor in the air. The colder the temperature, the less water vapor in the air.
Humidity happens when water vapor enters the air. It is suspended until it reaches such a saturation that it is released in the form of precipitation.
No, the more water vapor the air contains, the lighter it is. When water vapor enters the atmosphere, it pushes out an equal volume of dry air. A cubic meter of dry air is 99 percent nitrogen and oxygen. A cubic meter of humid air with 2 percent water vapor is only 97 percent nitrogen and oxygen. Water vapor is lighter than the nitrogen and oxygen it pushed out. Therefore, humid air weighs less than dry air and exerts less pressure.
The water is converted to water vapor and is carried out through the dryer vent by the air that flows through the machine.
The higher you go, the colder it gets. The colder it gets, the less water vapor can remain in the air. That's the reason it rains on the windward side of mountain ranges. Warm, moist air gets pushed up and the rain condenses.
Water enters the atmosphere and forms clouds primarily through the process of evaporation. When the sun heats bodies of water, the liquid water transforms into water vapor, which rises into the air. As the vapor cools at higher altitudes, it condenses around tiny particles, forming water droplets that cluster together to create clouds. This cycle is a key part of the Earth's water cycle, continuously moving water between the surface and the atmosphere.
Water vapor in the air returns to the surface through the process of condensation, where the vapor cools and turns back into liquid water. This can happen when the temperature drops, causing the vapor to condense and form clouds, eventually leading to precipitation in the form of rain or snow that falls back to the Earth's surface.
The mistiness inside a beaker can be due to condensation of water vapor when the temperature of the beaker is different from the surrounding air. This can occur when a warm beaker comes in contact with cooler air, causing water vapor in the air to condense on the inner surface of the beaker.