In cycling the Continental Divide in Colorado, you get a vivid picture of where much of our water comes from. During my long bike rides up there, I commonly find snow still melting in June. This snowmelt adds to streamflow that becomes our renewable water supply and my drinking water supply.
The part of rain and snowfall that does not naturally go back into the atmosphere becomes our water supply and it varies greatly across the United States. In the wettest regions, such as New England, precipitation is plentiful and about half of it ends up in streams or replenishes ground water supplies.
