The start of April marks the time when the western snowpack approaches its usual annual maximum. This winter brought record precipitation, including snowfall extremes from Seattle to Flagstaff, boosting this year’s snowpack totals. According to the USDA’s western SNOTEL network, this year’s end-of-season snowpack was above average for just the third time in ten years and the seventh time in twenty years. 2019’s overall western snowpack is 25 percent above the median normals, with especially high values in California, Arizona, and Nevada. Since snowmelt makes up around 75 percent of the West’s water supply, this above-average year will help farmers and city water users alike.
However, western snowpack is decreasing in the long term with human-caused climate change. Warmer air is turning potential snow into rain for some lower-elevation areas. Meanwhile, other areas are experiencing less precipitation overall, with that trend expected to continue. According to a December report from the University of Arizona, some western areas have recorded snowpack reductions of 41 percent in 35 years.
Western drought shows similar trends. This winter’s rain has helped ameliorate severe droughts in the current U.S. Drought Monitor. Still, it takes more than one rainy season to restore the groundwater that the West relies on. As we reported last month, drought and water deficits are projected to be the highest-risk climate impact for 40 percent of U.S. cities — including much of the West.
These droughts carry major costs, from intensifying wildfires to damaging crops that the nation depends on. Droughts have cost the U.S. billions of dollars every year since 2011, particularly in California which produces two-thirds of the nation’s fruits and nuts. Thank goodness the Golden State is nearly drought free — for now.