As water vapor rises into the troposphere, it cools and condenses into tiny water droplets or ice crystals, forming clouds. This process releases latent heat, which warms the surrounding air and can lead to further rising of air, contributing to convection currents. Eventually, the accumulated moisture may lead to precipitation, such as rain or snow, as the droplets coalesce and become heavy enough to fall back to the Earth's surface.
When the sun rises, the warmth and light cause the dew to evaporate. As the temperature rises, the water droplets in the dew transform into water vapor and are released into the air.
Clouds form in the sky when water vapor condenses into water droplets. This process happens when warm air rises, cools, and reaches its dew point, causing the water vapor to condense and form clouds.
When water rises into the air, it is called evaporation. Evaporation occurs when liquid water changes into water vapor due to heat energy from the sun.
The answer to the blank in the phrase "liquid water on Earth's surface _____ water vapor rises into the atmosphere" is "evaporates." When liquid water evaporates, it transforms into water vapor, which then rises into the atmosphere. This process is a key component of the water cycle, contributing to weather patterns and climate regulation.
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.
The troposphere can hold water vapor because it has the right temperature and pressure conditions for evaporation to occur. As air near the Earth's surface warms, it can hold more water vapor. When the warm air rises through the troposphere, it cools down, causing the water vapor to condense and form clouds and precipitation.
It becomes condensation.The water vapor turns into a liquid
The troposphere retains water vapor due to its ability to hold moisture in the form of invisible gas through processes like evaporation and transpiration from plants. As air rises, it cools and condenses, forming clouds and precipitation. This continuous cycle of evaporation, condensation, and precipitation helps maintain water vapor in the troposphere.
It condenses into liquid.
it will precipitate
it condenses
Water vapor is held by the troposphere in between molecules of atmospheric gases like oxygen, nitrogen and argon. Most of the water vapor in the troposphere is realized through transpiration off the earth's surface.
As water vapor cools to the dew point it converts from a gas back to a liquid.
Because air is cooler at higher altitudes in the troposphere, water vapor cools as it rises high in the atmosphere and transforms into water droplets by a process called condensation. The water droplets that form make up clouds.
Yes, the troposphere is the lowest layer of the Earth's atmosphere and contains air as well as varying amounts of water vapor. Water vapor plays a key role in the formation of weather patterns and cloud formation within the troposphere.
When the sun rises, the warmth and light cause the dew to evaporate. As the temperature rises, the water droplets in the dew transform into water vapor and are released into the air.
Clouds form in the upper troposphere. They form like this: Water on Earth's surface evaporates (turns into water vapor), and rises. When it gets to the upper troposphere, the water vapor starts turning back into water, staying as mist mostly, and mixes with dust. When the amount of water is to heavy, it starts to precipitate. Then, the precipitation evaporates on Earth's surface and the cycle begins again.