Few have forgotten the anguish of stunted crops and terror of devastating forest fires last year because of the meager snowpack that yielded paltry irrigation water and tinder-dry soils. The snowpack was far below normal last year, not for lack of precipitation (which was normal), but because of how unusually warm it was. Much more of the mountain precipitation fell as rain rather than snow.

Mountain snow is invaluable as a natural reservoir of water, storing winter precipitation for use during the dry growing season; 70 percent of runoff in the western U.S. is from snowmelt. Moreover, snow keeps the soil moist and vegetation green during summer, limiting the spread of forest fires when lightning strikes. It is the “lifeblood of the west” (Capital Press, Jan. 1, “Heavy snow eases Oregon drought concern, but uncertainties remain”).