yes
Water vapor in the air is visible in the form of mist, fog, and clouds.
Hail is formed in severe thunderstorms with strong updrafts that carry raindrops to high altitudes where they freeze. It is not always present in the atmosphere but occurs when specific conditions are met in thunderstorms.
The Earth's atmosphere contains about 0.001 of water in the form of water vapor.
The measure of the amount of water vapor in the atmosphere is called humidity. It is typically expressed as relative humidity, which is the ratio of the amount of water vapor present in the air to the maximum amount of water vapor the air can hold at a specific temperature.
In order for clouds to form, water vapor needs a surface to condense upon. This can be provided by tiny dust particles, salt particles, or other aerosols present in the atmosphere. These particles serve as nuclei around which water vapor can condense to form cloud droplets.
Water vapor in the air is visible in the form of mist, fog, and clouds.
Water vapor is always present in the air because water molecules are constantly evaporating from oceans, rivers, lakes, and other bodies of water, as well as from plants and soil. This constant evaporation releases water vapor into the atmosphere, where it can remain suspended as humidity in the air.
Hail is formed in severe thunderstorms with strong updrafts that carry raindrops to high altitudes where they freeze. It is not always present in the atmosphere but occurs when specific conditions are met in thunderstorms.
The Earth's atmosphere contains about 0.001 of water in the form of water vapor.
water vapor and condensation
A hygrometer is used to measure water vapor in the atmosphere. This instrument can measure humidity levels in the air to determine the amount of water vapor present.
water vapor is one of the greenhouse gases that is present around the planet and helps reflect heat back to Earth's surface , keeping it within the atmosphere.
The measure of the amount of water vapor in the atmosphere is called humidity. It is typically expressed as relative humidity, which is the ratio of the amount of water vapor present in the air to the maximum amount of water vapor the air can hold at a specific temperature.
In order for clouds to form, water vapor needs a surface to condense upon. This can be provided by tiny dust particles, salt particles, or other aerosols present in the atmosphere. These particles serve as nuclei around which water vapor can condense to form cloud droplets.
The term for the amount of water in the atmosphere is humidity. Humidity is typically measured as either relative humidity, which is the percentage of water vapor present in the air compared to the maximum amount the air can hold at a specific temperature, or absolute humidity, which is the actual amount of water vapor present in the air.
Yes, water vapor is present in the atmosphere at all times, including nighttime. The amount of water vapor in the air can vary depending on factors such as temperature, humidity, and weather conditions.
The instrument used to measure the amount of water vapor in the atmosphere is called a hygrometer. It works by calculating the humidity levels in the air based on factors like temperature and the amount of water vapor present.