TUCSON – Northeastern Arizona no longer is dealing with extreme drought, thanks to ample fall and winter precipitation, making this season’s snowpack one of the most abundant in awhile, the Arizona Department of Water Resources reports.
In addition, it said, soil beneath the snow is saturated, which means there should be significant spring runoff to partially replenish the streams, rivers and reservoirs on which the West depends. As of this week, 73 percent of Arizona was deemed free of drought, although the Four Corners area remains in severe drought.
Researchers at the University of Arizona are working to find better ways to track snowpack in Arizona and across the U.S. The team has been collecting snowpack data since 1981, and they now can map changes in snow mass across the country over the past 35 years onto grids that are 2.5 square miles.
Professor Xubin Zeng, who leads this work, said the results will change how people track snowpack in the future to better deal with diminished water sources in the warming and drying West.
“Before, we only have good measurements of our specific points, say your own backyard,” Zeng said. “Now if you want to tell your neighbors what is snowpack change for your neighborhood and adjacent areas, you don’t know because your backyard could be different from your neighbor’s. Not for your backyard but for your neighborhood and surrounding areas, and we can do that for every neighborhood in the U.S.”
There are tens of thousands of volunteers across the country measuring snowpack. Zeng said he and his fellow researchers have combined that information with government measurements to create a consistent data set that can give greater detail on snowpack than historical ways of measuring snow. All this information is used to map the snowpack on every inch of land in the U.S., which has not been done before.
Zeng’s team has discovered that although snowpack in the eastern U.S. is doing well, it has diminished across the West. In fact, it has declined so much that if all that snowpack was combined together, it would be about the size of South Carolina.
Snow water equivalent, or SWE, describes how much water is in snowpack. Declining SWE is strongly correlated with long-term climate change. Climate Signals, a science information project of the nonprofit Climate Nexus, said human-caused global warming is the main cause for reduced snow cover.
According to the National Centers for Environmental Information, this winter has been the wettest on record for the contiguous U.S. Precipitation amounts have increased lately, and it has been colder in many parts of the country.