California Snowlines On Track To Be 1,600 Feet Higher by Century’s End
California Snowlines On Track To Be 1,600 Feet Higher by Century’s End
May 30, 2023
Reno, Nev.
Shared with permission from Scripps Institution of Oceanography
Snowpack
Climate Change
DRI contributes to research concluding lower-elevation ski resorts could lose more than 70 percent of their natural snow supply
DRI’s Benjamin Hatchett, Ph.D, and Michael Dettinger, Ph.D., coauthored a new study in the journal Climate Dynamics that predicts dramatic changes for California’s future snowpack. The team combined seven decades of temperature and precipitation data with projections about climate change to examine the growing impact of atmospheric rivers, which tend to be warmer than other storms. With less snow in California’s future, there will be wide-ranging impacts on landscapes, ecosystems, and water availability for human communities.
“The snowline is an iconic component of mountains,” Hatchett says. “Its warming-driven upslope retreat poses numerous implications for the aspects of mountain environments we rely on for water resources, ecosystem function, and recreation. As the snowline moves upslope, increased winter runoff will occur at the expense of spring runoff, a change our current water management paradigm is not designed for. A longer snow-free environment will promote more severe wildfire activity at higher elevations and the numerous cascading impacts severe wildfire brings to ecosystems, life and property, and public health. Last, we will see recreation impacts such as shorter ski seasons, less available skiable terrain, and lower flows during the summer and fall, which when combined with other climate change impacts, negatively affects mountain economies.”
Below is the full press release from Scripps Institution of Oceanography.
San Diego – March 25, 2023 –
This winter produced record snowfall in California, but a new study suggests the state should expect gradually declining snowpacks, even if punctuated with occasional epic snowfalls, in the future.
An analysis by Tamara Shulgina, Alexander Gershunov, and other climate scientists at UC San Diego’s Scripps Institution of Oceanography suggest that in the face of unabated global warming, the snowlines marking where rainfall turns to snow have been rising significantly over the past 70 years. Projections by the researchers suggest the trend will continue with snowlines rising hundreds of meters higher by the second half of this century.
In the high Southern Sierra Nevada range, for instance, snowlines are projected to rise by more than 500 meters (1,600 feet) and even more when the mountains get precipitation from atmospheric rivers, jets of water vapor that are becoming an increasingly potent source of the state’s water supply.
“In an average year, the snowpack will be increasingly confined to the peak of winter and to the highest elevations,” the study says.
Diminished snowfall is a consequence of a changing climate in which places like California will get an increasing portion of their winter precipitation as rain instead of snow. The authors said this study and related research suggest water resource managers will need to adapt to a feast-or-famine future. California’s water supply will arrive less through the gradual melt of mountain snowpack that gets the state through hot summers and more via bursts of rain and runoff delivered by atmospheric rivers, which are boosted by warming and are associated with higher snowlines than other storms.
Such events will further complicate the balancing act between protecting people and infrastructure from winter flooding and ensuring enough water supply during warmer summers.
“This work adds insight into the climate change narrative of more rain and less snow,” said California Department of Water Resources (DWR) Climatologist Mike Anderson. “DWR appreciates our partnership with Scripps to help water managers develop, refine, and implement adaptation efforts as the world continues to warm and climate change impacts are realized.”
The study, funded by the U.S. Bureau of Reclamation and the DWR, appears in the journal Climate Dynamics.
“This is the longest and most detailed account of snow accumulation in California,” said Gershunov, “resolving individual storms over 70 years of observed weather combined with projections out to 2100.”
The authors make note of what this could mean for ski resorts around the state if climate change progresses unabated. For example, Mammoth Mountain, at an elevation between 2,400 and 3,300 meters (7,900 – 11,000 feet), is projected to receive 28 percent less snowfall in the latter half of the century. Lower elevation ski resorts such as Palisades and Northstar, both near Lake Tahoe, span elevational ranges of around 1,900 and 2,700 meters (6,200 – 8,900 feet). They are projected to lose more than 70 percent of their snow accumulation in an average winter.
“Observations and future climate projections show that already rising snowlines will keep lifting,” said Gershunov. “Epic winters will still be possible, though, and unprecedented snowfalls will ironically become more likely due to wetter atmospheric rivers, but they will be increasingly confined to the peak of winter and to the highest elevations of the Southern Sierra Nevada.”
Study co-authors include Kristen Guirguis, Daniel Cayan, David Pierce, Michael Dettinger, and F. Martin Ralph of Scripps Oceanography, Benjamin Hatchett of the Desert Research Institute of Reno, Nev., Aneesh Subramanian of University of Colorado at Boulder, Steven Margulis and Yiwen Fang of UCLA, and Michael L. Anderson of the California Department of Water Resources.
