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Sierra Nevada is a Spanish name that means “snowy mountain range.” While the term “snowy” has generally been true for most of American history, the mountain range has seen far less snow accumulation in recent years.
The depth and breadth of the seasonal snowpack in any given year depends on whether a winter is wet or dry. Wet winters (such as 2017) tend to stack up a deep snowpack, while dry ones keep it shallow. In 2015, long-term hot and dry conditions in California and Nevada brought snowpack to historically low levels.
This series of images shows the snowpack on the Sierra Nevada from 2006 to 2017. The natural-color images were acquired by the Moderate Resolution Imaging Spectroradiometer (MODIS) on NASA’s Terra satellite. Each image was acquired around April 1, halfway through the water year. A “water year” is the 12-month period from October 1 through September 30. The snowpack on the Sierra Nevada has generally peaked and begins to melt by the beginning of April. Meltwater runoff from that snowpack helps replenish rivers and reservoirs while recharging the groundwater.
The series begins in 2006, which was a wet year with substantial snowfall. Then dry water years struck from 2007–2009—the first time in California’s history that statewide declarations of emergency were issued for drought, according to the California Department of Water Resources. In 2009, the proclamation noted that rainfall and snowpack deficits were putting California “further and further behind in meeting its essential water needs.”
Wet years returned from 2010–2011. The wet year of 2011 buffered the initial effects of drought that returned in 2012, but dry conditions deepened in subsequent years. By March 2015, about one-third of the ground-based monitoring sites in the Sierra Nevada recorded the lowest snowpack ever measured. Some sites reported no snow for the first time. One month later, only some sites—generally those at higher elevations—had any measureable snowpack.
Scientists from the University of Arizona wrote in a September 2015 article in Nature Climate Change that the low snowpack conditions of 2015 were truly extraordinary. Tree-ring records of precipitation anomalies and of temperature allowed them to reconstruct a 500-year history of snow water equivalent in the Sierra Nevada. The researchers found that the low snowpack of April 2015 was “unprecedented in the context of the past 500 years.”
El Niño conditions in 2015-16 brought substantial rain and snowfall back to the mountains, but snow cover still fell short of long-term averages. Then a steady stream of atmospheric river events brought double the long-term average of rain and snow to the Sierra Nevada between October 2016 and April 2017.