In his final State of the Union address, President Obama put more emphasis on climate change than ever before . Scientists no longer dispute the fact that humans are having an impact on the earth, and global leaders have come to an agreement that involves taking actions to fight climate change and mitigate its negative effects .
The impacts of climate change are already visible around the world, from extreme storms and fluctuating temperatures, to long droughts and threatened agricultural productivity. These changes are difficult to predict because modern civilization has never experienced any periods of such extreme warming. However, polar ice is indisputably melting faster than it can be replenished by snowfall accumulation , and governments all over the world are already preparing for and combating sea level rise.
So, how will climate change and sea level rise impact the drying Salton Sea?
Prehistorically, we know that the Salton basin was occupied by Lake Cahuilla, which was part of the greater Colorado River basin. However, the Colorado River delta silted up over time, eventually leaving ancient lakebeds, such as the Salton Sink and Laguna Salada, sitting far below sea level without any connection to or from the ocean.
Over the last century, annual sea level rise has doubled and still continues to accelerate . Sea level rise is the result of a combination of:
- Thermal expansion: As ocean water gets warmer, it is able to store more heat energy and thus take up more volume.
- Glacial melt: As temperatures in polar regions increase, glaciers that are currently solid ice on land will eventually melt, and increase the liquid volume in the ocean.
Unfortunately, variables like ocean salinity and local temperature differences make it difficult to estimate the rates and extent that each of these changes will occur .
In 2013, the National Climate Assessment, conducted by NASA, released models of predicted global temperature change by 2100 . In their best-case scenario (B1, in the video below), in which actions are taken to globally reduce environmental impacts, different parts of the world will experience between 2° and 5°F of warming. In the worst-case scenario (A2, in the video below), in which global development continues while ignoring environmental impacts, some parts of the world could see nearly 15°F increases by 2100. At that point, the Salton Sea would be well on its way to connecting with the Sea of Cortez.
NASA visualization of predicted changes in annual and summer temperature, based on the best- and worst-case carbon emission scenarios .
While the rate of change is difficult to accurately predict for the relatively short-term future, what we do know is that our actions during this century will essentially lock in the increased sea levels at some point in the future. Carbon persists in the atmosphere and continues to affect the earth long after it is emitted. This means that even if we stopped burning fossil fuels today, the sea level will continue to rise for hundreds and thousands of years.
It would take about 30 feet of sea level rise to connect the Salton Sink to the ocean and permanently fill it again. Realistically, climatologists expect at most 2 meters (about 6.5 feet) of sea level rise by 2100. But, you can play with sea level change models like this one and see that without significant reductions to our carbon emissions and/or physical intervention to block sea level rise, the Salton Sink (as well as all of the area reaching from Imperial Valley to the Sea of Cortez) will eventually be permanently under water.
What will be the repercussions of increasing temperatures and sea levels as it pertains to the Salton Sea? Let us know what you think in the comments, and we’ll be back with another post on the various potential consequences soon!
 Dokoupil, T., Obama goes big on climate change. MSNBC, January 12, 2016. Available at http://www.msnbc.com/msnbc/obama-goes-big-climate-change
 United Nations Conference on Climate Change, More details about the agreement. Available at http://www.cop21.gouv.fr/en/more-details-about-the-agreement/
 Schoenherr, Allan A., A Natural History of California. University of California Press, New York, NY, 1995.
 National Climate Assessment: 21st Century Temperature Scenarios. Visualizations by Greg Shirah. March 7, 2013. Available at http://svs.gsfc.nasa.gov/cgi-bin/details.cgi?aid=4029
 Strauss, B.H., Kulp, S., Lenermann, A. (2015) Carbon choices determine U.S. cities committeed to futures below sea level. Proceedings of the National Academy of Sciences, 112, 44 (13508-13513). Available at http://www.pnas.org/content/112/44/13508
 Pfeffer, W.T., Harper, J.T., O’Neel, S. (2008) Kinematic contraints on glacier contributions to 21st-century sea-level rise. Science, 321, 5894 (1340-1343). Available at http://science.sciencemag.org/content/321/5894/1340
 San Diego State University Center for Inland Waters. Salton Basin-Colorado Delta Mothersite. Available at http://www.sci.sdsu.edu/salton/SaltonBasinHomePage.html