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Saturday, April 4, 2015

Another Trenberth travesty,

Another Trenberth travesty

In all storms, the main source of precipitation is the moisture already in the atmosphere at the start of the storm. This moisture, as water vapor, is gathered by the storm winds, brought into the storm, concentrated and precipitated out. Accordingly, if there is more moisture in the environment, it rains (or snows) harder.
How does this play out when temperatures are below freezing? Temperatures in the Goldilocks range of between about 28°F and 32°F, accompanied by moisture, mean more snow: indeed, the amount of snowfall at 32°F would be at least double that at 14°F.

paper

paper

"the extra snow can easily be order 10% or more"

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