Originally Posted By: M_a_x
As a ball park number you could assume that - in arid areas - 1 m³ of air has less than 10 ml³ of water as vapour.


The atmosphere certainly can be dry at times, but it can also be quite humid, without inducing any precipitation. In my experience, primarily in the deserts of the American Southwest, early morning dew is not at all uncommon.

I'll be curious to see how this technology develops. Even if it proves feasible, I would prefer a nice gushing spring. Who wouldn't? But this could be a big help....
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