Hydropower Generation Projected to Rise, but Climate Change Brings Uncertain Future
The researchers teamed up with colleagues at DOE’s Oak Ridge National Laboratory, who have developed models that show how climate change might alter the timing and volume of water flow in streams and rivers over the next few decades. The PNNL team then ran that water flow data through models that captured the multiple uses of water and calculated hydropower generation for two time periods: a near-term period spanning 2020–2039 and a midterm period spanning 2040–2059.
The team found that hydropower production generally increases about 5% in the near term and 10% in the midterm across the continental United States. This could be because climate models generally show an increase in precipitation as Earth warms.
Only one part of the country saw an average decrease in hydropower generation: in some parts of the Southwest, which is already facing drought, the models project a slight decrease in hydropower production between 3–6% in the near term.
Broman stressed that because the future of climate change is uncertain, the range of possible outcomes for hydropower generation is large. For example, between 2020–2039, hydropower generation could change between –5–21% while in later years it could change –4–28%.
Seasonal changes could also have big implications for how water is managed across the country, Broman said.
Hydropower Changes by Season
In the winter, the team found that hydropower generation may rise 12% in the near term and 18% in the midterm across the United States. Similarly, increased rainfall during the fall may lead to a near-term 5–20% rise in hydropower production in the Southeast, as well as smaller increases in the Northeast and Midwest.
But some of the biggest hydropower generation changes may occur in the summer, especially in the West. In the summer, hydropower generation may decrease 1–5% in the western region of the country, while higher precipitation may increase hydropower generation in the eastern areas by 1–5%, both in the near-term.
Historically, mountain snowpack in the West has stored water until the late spring and summer. When the snow melts, that water generates more electricity. Now, due to increased temperatures, less snow accumulates on mountains and melts earlier in the year. The early snowmelt and shift toward rain in the winter means hydropower generates more electricity during the winter and less in the following spring and summer.
“Snow is storage. If the snow melts earlier, it changes the timing and volume of water availability,” Voisin said. “And because temperatures are rising overall, the hydropower availability and energy demand might not be in sync.”
The Future of Hydropower
Voisin stressed that even if hydropower generation declines in certain seasons, it still offers a reliable source of energy for the power grid. Like a coal or gas plant, hydropower can be dispatched as needed and provide stability to the grid as a whole—highlighting its flexibility as a renewable energy source.
Broman and Voisin hope that power system operators and water managers can use the new consistent multiscale assessment and the accompanying data to inform water-energy tradeoffs discussions, such as hydropower flexibility needs amid other societal benefits of water uses.
With climate change bringing an uncertain future, historical records don’t necessarily reflect what the next few decades may bring, Broman said. What’s more, “utilities may be thinking about hydropower generation under climate change for their own region, but the electricity grid is bigger than that.”
JoAnna Wendel is Media Relations Specialist at the Pacific Northwest National Laboratory (PNNL). The articlewas originally posted to the website of PNNL.
