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The strength of the rainfall within it, though, is likely to rise, because the air will be warmer, and warmer air can hold more water.
Warmer air and less snowmelt would mean a much warmer river and depleted soil moisture in summer, which would stress forest vegetation.
Warmer air has a higher saturation level.
Warmer air holds more water vapour.
It was trapped by the warmer air above.
Another could be that warmer air is often moister.
This occurs because cold air tends to undercut the warmer air of tropical origin.
Evidence of this overturn is produced in the form of bubbles, or eddies, of warmer air.
Some cold places will see more snow, because warmer air can carry more moisture.
Under such conditions the cooler air tends to sink, displacing the warmer air upward.
As our climate warms, atmospheric rivers will become stronger, because warmer air can carry more moisture.
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