New climate research reveals growing risk of water shortages and flooding in California
If the world continues to burn greenhouse gases, California may have an increased risk of winter floods and summer water shortages, even within the same year. This scenario may be more severe in future El Ni帽o years.
New research by Lawrence Livermore National Laboratory (LLNL) scientists shows that global warming is likely to change river flows in ways that may result in both increased flood risk and water shortages. The predictions assume atmospheric carbon dioxide concentration doubles from preindustrial levels.
The amount of water flowing in California鈥檚 rivers needs to be just right. Too much brings a risk of flooding; too little causes reservoir levels to drop.
As temperatures warm as a result of carbon emission, more rain than snow falls at higher elevations. For the areas that do receive snow, melt occurs sooner.
The research shows that this well-known scenario 鈥� in which global warming causes an increase in wintertime river flows and a reduction in spring and summer flows 鈥� is more robust than previously thought.
鈥淚t seems unlikely that any changes in precipitation will be large enough to eliminate these problems,鈥� said Philip Duffy, an LLNL physicist and director of the Institute for Research on Climate Change and its Societal Impacts, a University of California Intercampus Research Program. Furthermore, in an El Ni帽o (a naturally occurring climate fluctuation) season, these problems may be more severe.
California鈥檚 water infrastructure is very efficient at providing an adequate water supply and minimizing flood risk. The system, however, works well only in a climate that includes large amounts of mountain snow. Melting snow keeps reservoirs full in the late spring and summer, after rain and snowfall have stopped. Snow acts as a natural reservoir, with a volume close to that of manmade reservoirs.
As global warming ensues, more precipitation will be in the form of rain rather than snow. Also, what snow remains will melt earlier in the year. These changes will result in higher river flow rates in California鈥檚 major rivers during winter and lower flows during spring and summer, when flows are largely from snowmelt.
鈥淓ven if total flows over the whole year are the same, these changes could jeopardize water supplies, because it may not be possible for reservoirs to capture the increased winter flows,鈥� said Edwin Maurer, a professor at Santa Clara University and lead author of the research that appears in the Jan. 27 edition of the journal Geophysical Research Letters. 鈥淭his problem would be compounded by an increased risk of wintertime flooding resulting from higher river flow rates,鈥� he said.
This would force water managers to reduce reservoir water levels to provide extra space for capturing increased winter flood surges, which would further reduce the overall year鈥檚 water supply.
鈥淚n an El Ni帽o year, which brings more rain than a typical year, there would be an increase (versus today) in the year-to-year variability in river flow rates, which would make life complicated for people who manage the water supply,鈥� Duffy said.
The researchers simulated only monthly mean river flows, so they can鈥檛 quantitatively assess flood risk, which depends on daily-timescale river flows. However, the monthly flows are high enough to indicate that flood risk would be much higher.
鈥淚n particular, there will be increased wintertime river flows and lower spring and summer flows whether future precipitation increases or decreases modestly,鈥� Maurer said. 鈥淚t seems unlikely that the potential problems can be avoided by changes in precipitation.鈥� This finding was published earlier this year by Maurer and Duffy.
The newest paper by Maurer, Duffy, and Seran Gibbard of LLNL鈥檚 AX Division investigates effects on California river flows of a hypothetical future-climate El Ni脩o. El Ni脩o is a naturally occurring climate oscillation that typically produces increased precipitation, river flows and flood risk in California.
The team鈥檚 work has some limitations: The researchers assumed that the strength of an El Ni帽o, as measured by departures of sea-surface temperatures from long-term average values, will be the same in the future as today. They did this because climate models don鈥檛 agree on how the strength of an El Ni帽o is likely to change.
Source: Lawrence Livermore National Laboratory
