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Closer to the ground, the water vapour content also changes with height in a regular pattern.
In a warming world, atmospheric water vapour content is expected to rise … with air temperature.
Also, atmospheric water vapour content is higher near the source of moisture than in distant regions.
Moreover, the higher the vapour content of the atmosphere, the more latent energy is available for the generation of storms.
The greater water vapour content of a warmer atmosphere allows larger rainfall anomalies and provides the fuel for stronger storms driven by latent heat.
Dew point, the temperature at which the atmosphere is saturated with water vapour, when it is cooled without changing its pressure or vapour content.
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As the warm, humid air cools in the tube the vapour contents condense to form water.
Many industrial gas separations in which membrane processes are feasible entail high water vapour contents, as in CO2-separation from flue gas in carbon capture and storage (CCS), or in biogas/natural gas processing.
Relative humidity is the water-vapour content of the air relative to its content at saturation.
The water-vapour content of the atmosphere varies from place to place and from time to time because the humidity capacity of air is determined by temperature.
Sodium is ordinarily quite reactive with air, and the reactivity is a function of the relative humidity, or water-vapour content of the air.
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