29 August 2017
WASHINGTON D.C. — Earth’s largest inland body of water has been slowly evaporating for the past two decades due to rising temperatures associated with climate change, a new study finds.
Water levels in the Caspian Sea dropped nearly 7 centimeters (3 inches) per year from 1996 to 2015, or nearly 1.5 meters (5 feet) total, according to the new study. The current Caspian Sea level is only about 1 meter (3 feet) above the historic low level it reached in the late 1970s.
Increased evaporation over the Caspian Sea has been linked to increased surface air temperatures. According to the data from the study, the average yearly surface temperature over the Caspian Sea rose by about 1 degree Celsius (1.8 degrees Fahrenheit) between the two time frames studied, 1979-1995 and 1996-2015. These rising temperatures are likely a result of climate change, according to the study’s authors.
Evaporation brought about by warming temperatures appears to be the primary cause of the current drop in sea level and the decline will likely continue as the planet warms, according to the study’s authors.
“From our point of view as geoscientists, it’s an interesting place because it’s possible to construct a sort of budget for the total amount of water that’s there,” said Clark Wilson, a geophysicist with the Jackson School of Geosciences at the University of Texas at Austin, and co-author of the new study published in Geophysical Research Letters, a journal of the American Geophysical Union. “The real control that causes it to go up and down over long periods of time is really most likely the evaporation, which is almost completely dominated by temperature.”
The Caspian Sea, located between Europe and Asia, is roughly the size of Montana at 371,000 square kilometers (143,244 square miles). It has experienced substantial changes in its water level over the past several hundred years, but previous studies were unable to nail down the exact causes of the sea level changes.
The Caspian Sea is bordered by five countries and contains an abundance of natural resources and diverse wildlife. The sea also contains oil and natural gas reserves, and is an important resource for fisheries in the surrounding countries.
The new study began after Wilson and Jianli Chen, the study’s lead author from the Center for Space Research at the University of Texas at Austin, along with other researchers, used the Caspian Sea to calibrate data from the twin satellites of the GRACE mission launched in 2002. By comparing measurements of the Caspian Sea from GRACE data and Earth-based measurements, the researchers helped improve the satellite data’s accuracy. In doing so, they noticed the Caspian Sea’s water levels were undergoing significant changes.
“Once we got through with [the calibration], Jianli Chen said, ‘Well, you know, this is very curious. Why is this changing so much?’” Wilson said. “That got us going on the current question, which is trying to understand what the reason is for these multimeter variations in the sea level. It’s an interesting place, and it’s been studied for a long time, but it wasn’t really clear.”
The researchers looked at the three primary influences on Caspian Sea water levels: water from rivers that drain into the sea, precipitation and evaporation.
They compiled information about water level changes observed by satellites, records of precipitation and drainage into the sea from rivers, and estimations of precipitation and evaporation from climate models. The researchers then assembled a record of how much each of these factors contributed to observed changes in the Caspian Sea level from 1979 to 2015.
They found Caspian Sea levels increased by about 12 centimeters (5 inches) per year from 1979-1995. But in 1996, sea levels began to drop, and declined by an average of nearly 7 centimeters (3 inches) per year through 2015. From 1996-2015, the Caspian Sea level dropped nearly 1.4 meters (4.5 feet), according to sea level records used in the study.
Evaporation contributed to about half of that decline, while the combined effects of precipitation and river discharge changes contributed to the other half. According to the study, the observed evaporation rates are associated with increased surface air temperature and other climate factors such as surface humidity and wind.
The new study provides the first convincing evidence that increased evaporation over the Caspian Sea is a more important driving force of Caspian sea level change than river discharge or precipitation, said Anny Cazenave, a CNES space geodesist at the Laboratoire d’Etudes en Géophysique et Océanographie Spatiales (LEGOS) at Observatoire Midi-Pyrénées in Toulouse, France, who was not involved in the new study.
“An interesting finding from the study is that over the last two decades, climate-model predicted water loss … apparently cannot be balanced by water gain from discharge, and increased evaporation is a major factor leading to this imbalance,” Cazenave said. “If the temperature in the Caspian Sea region continues to increase, the evaporation rate is also expected to increase. Unless river discharge increases accordingly or precipitation in the Caspian drainage basin increases accordingly, the imbalance is likely to continue.”
The Caspian reached a historic low of 29 meters (95 feet) below mean sea level in the late 1970s before water levels increased in 1978. If current evaporation rates continue, the results suggest the sea could approach the historic low again, according to the study’s authors.
Evaporation will have the biggest impact on the northern portion of the Caspian Sea because much of the water in that area is less than 5 meters (16 feet) deep, Wilson said. If the current trend of a 7-centimeter decrease per year continues at a steady rate, it would take around 75 years for the northern part of the sea to disappear, according to the new study.
The Caspian Sea supports many unique and ancient species remaining from when the sea was a part of the Tethys Ocean during the Mesozoic era, approximately 300 million years ago. Although most of these species live in the southern and middle regions of the Caspian, some use the shallow northern area as spawning grounds, including 90 percent of the world’s sturgeons. Dropping sea levels would also impact the Kara-Bogaz-Gol Bay on the eastern side of the sea, which is less than 5 meters (16 feet) deep and contains one of the world’s largest natural deposit of sea salts, according to the study’s authors.
Wilson said the next step in this research is to project future changes in Caspian Sea level using climate models. Although this study identified the trends in sea level and their causes, the researchers did not project specific estimates of how these levels might change in the future.
“If you’re going to take this to the next step, it would be to take a suite of climate models or look at some sort of ensemble predictions of future temperatures to get some idea of what those scenarios might be for the Caspian Sea,” Wilson said. “You can imagine if you had a continued decline in sea level that led to several meters of loss, you’ve considerably diminished the size of the sea.”
The American Geophysical Union is dedicated to advancing the Earth and space sciences for the benefit of humanity through its scholarly publications, conferences, and outreach programs. AGU is a not-for-profit, professional, scientific organization representing 60,000 members in 137 countries. Join the conversation on Facebook, Twitter, YouTube, and our other social media channels.
Notes for Journalists
This research article is open access for 30 days. A PDF copy of the article can be downloaded at the following link: http://onlinelibrary.wiley.com/doi/10.1002/2017GL073958/pdf.
Journalists and PIOs may also order a copy of the final paper by emailing a request to Lauren Lipuma at [email protected]. Please provide your name, the name of your publication, and your phone number.
Neither the paper nor this press release is under embargo.
“Long-term Caspian Sea level change”
Jianli Chen: Center for Space Research, University of Texas at Austin, Austin, Texas, U.S.A.;
Tatyana Pekker: Center for Space Research, University of Texas at Austin, Austin, Texas, U.S.A.;
Clark R. Wilson: Center for Space Research, University of Texas at Austin, Austin, Texas, U.S.A. and Jackson School of Geosciences, University of Texas at Austin, Austin, Texas, U.S.A.;
Byron D. Tapley: Center for Space Research, University of Texas at Austin, Austin, Texas, U.S.A
Andrey G. Kostianoy: P.P. Shirshov Institute of Oceanology, Moscow, Russia and Laboratory of Integrated Studies of Water Resources, S.Yu. Witte Moscow University, Moscow, Russia;
Jean-François Cretaux: Laboratoire d’Etudes en Géophysique et Océanographie Spatiales, Toulouse, France;
Elnur S. Safarov: Department of the Caspian Sea Level Problem, Institute of Geography, Baku, Azerbaijan, Baku, Azerbaijan.
Contact information for the authors:
Jianli Chen: [email protected], +1 (512) 232-6218
+1 (202) 777-7396
University of Texas at Austin Press Contact:
+1 (512) 232-9623