According to the USGS and NOAA, a 1km³ cumulus cloud would weigh about 2.21 billion pounds, or about 1,105 tons (US). The same volume of dry air weighs about 2.22 billion pounds, which is why clouds float. Because it is less dense than air, in truth, it doesn't "weigh" anything. It has volume. If you sucked all the water vapor out of the air and put it in a bucket, though, using the below chart as a guide and the fact that water is 1kg per liter, and one liter of water is 0.1 cubic meters, you'd have 12,900,000,000 liters of water, which is 12.9 trillion kg. (It's enough to cover the earth's 510,072,000 km² surface with about 25mm of water. Because the earth's average rain fall is about 1 meter, you can figure that all of this water vapor is recycled every nine or ten days.) So, to convert that metric to US tons and answer your question, all of that means that there is approximately more than 14.2 billion US tons of water vapor in the atmosphere.
Water sourceWater volume, in cubic milesWater volume, in cubic kilometersPercent of total freshwaterPercent of total waterAtmosphere3,09412,9000.04%0.001%Total global fresh water8,404,00035,030,000100%2.5%Total global water332,500,0001,386,000,000--100%Source: Gleick, P. H., 1996: Water resources. In Encyclopedia of Climate and Weather, ed. by S. H. Schneider, Oxford University Press, New York, vol. 2, pp.817-823.
The stratosphere contains almost no water vapor.
Water vapor is present in very low concentrations in the upper stratosphere, primarily from transport processes and chemical reactions in the lower atmosphere. It plays a role in stratospheric chemistry and has implications for ozone depletion.
Water vapor can be transported into the stratosphere through processes like deep convection or during the formation of high-altitude clouds. Once in the stratosphere, it can be trapped due to temperature inversions that prevent vertical mixing, leading to its accumulation in that layer of the atmosphere.
The stratosphere is typically cold. Temperatures generally decrease with altitude in the stratosphere due to the low concentration of water vapor and presence of ozone, which absorbs and retains heat.
The ratio of water vapor in a volume of air relative to how much water vapor that volume of air is capable of holding is called relative humidity. It is expressed as a percentage and provides insight into how close the air is to being saturated with water vapor.
The amount of water vapor in the stratosphere is much lower than in the lower atmosphere. The condensation of water vapor is what creates clouds (and rain, hail, snow, and other forms of precipitation) Also because weather occurs in the troposphere, and clouds are formed from water vapor, which is part of the water cycle, which is part of weather
The stratosphere contains almost no water vapor.
Water vapor is present in very low concentrations in the upper stratosphere, primarily from transport processes and chemical reactions in the lower atmosphere. It plays a role in stratospheric chemistry and has implications for ozone depletion.
There is no rain in the stratosphere because the amount of water in the stratosphere is much lower than in the lower atmosphere, which means the condensation of water vapour which creates rain doesn't occur in the atmosphere.
Water vapor can be transported into the stratosphere through processes like deep convection or during the formation of high-altitude clouds. Once in the stratosphere, it can be trapped due to temperature inversions that prevent vertical mixing, leading to its accumulation in that layer of the atmosphere.
The stratosphere is composed primarily of nitrogen and oxygen, similar to the composition of the lower atmosphere. However, the stratosphere contains much lower concentrations of water vapor and higher concentrations of ozone, which is crucial for absorbing the Sun's harmful ultraviolet radiation.
The stratosphere is primarily composed of nitrogen (about 78%) and oxygen (about 21%). It also contains trace amounts of other gases such as ozone, water vapor, and carbon dioxide.
The stratosphere is typically cold. Temperatures generally decrease with altitude in the stratosphere due to the low concentration of water vapor and presence of ozone, which absorbs and retains heat.
The ratio of water vapor in a volume of air relative to how much water vapor that volume of air is capable of holding is called relative humidity. It is expressed as a percentage and provides insight into how close the air is to being saturated with water vapor.
Yes, water vapor does have mass. Water vapor is a gas composed of water molecules, and like all matter, it has mass. However, the mass of water vapor is much lighter compared to liquid water.
The stratosphere contains various gases, with the most abundant being ozone. Ozone plays a vital role in absorbing the sun's harmful ultraviolet radiation, making the stratosphere crucial for protecting life on Earth. Other gases found in the stratosphere include nitrogen, oxygen, water vapor, and trace amounts of greenhouse gases like methane and carbon dioxide.
Water vapor is naturally present in the Earth's atmosphere and plays a key role in the water cycle. CFCs (chlorofluorocarbons) are used in refrigeration, air conditioning, and aerosol propellants. However, CFCs have been found to deplete the ozone layer in the stratosphere, leading to the implementation of regulations to phase them out.