19 August 2013
BOULDER – When enough raindrops fall over land instead of the ocean, they begin to add up.
New research shows that in 2010 and 2011, enough water collected in Australia to temporarily halt a long-term trend of global sea level rise. When three atmospheric patterns came together over the Indian and Pacific oceans in 2010-11, they drove so much precipitation over Australia that the world’s ocean levels dropped measurably. Unlike other continents, the soils and topography of Australia prevent almost all of its precipitation from running off into the ocean.
Now that the atmospheric patterns have snapped back and more rain is falling over tropical oceans, the seas are rising again. In fact, with Australia in a major drought, they are rising faster than before.
“It’s a beautiful illustration of how complicated our climate system is,” says John Fasullo, the lead author of the study. “The smallest continent in the world can affect sea level worldwide. Its influence is so strong that it can temporarily overcome the background trend of rising sea levels that we see with climate change.”
The study led by the National Center for Atmospheric Research (NCAR), with co-authors from NASA’s Jet Propulsion Laboratory and the University of Colorado at Boulder, will be published next month in Geophysical Research Letters.
Consistent rising, interrupted
As the climate warms, the world’s oceans rose in recent decades by just more than 3 millimeters (0.1 inches) annually. This is partly because the heat causes water to expand, and partly because runoff from retreating glaciers and ice sheets is making its way into the oceans.
But for an 18-month period beginning in 2010, the oceans mysteriously dropped by about 7 millimeters (about 0.3 inches), more than offsetting the annual rise.
Fasullo and his co-authors published research last year demonstrating that the reason had to do with the increased rainfall over tropical continents. They also showed that the drop coincided with the atmospheric oscillation known as La Niña, which cooled tropical surface waters in the eastern Pacific and suppressed rainfall there while enhancing it over portions of the tropical Pacific, Africa, South America, and Australia.
But an analysis of the historical record showed that past La Niña events only rarely accompanied such a pronounced drop in sea level.
Using a combination of satellite instruments and other tools, the new study finds that the picture in 2010–11 was uniquely complex. A rare combination of two other semi-cyclic climate modes came together to drive such large amounts of rain over Australia that the continent, on average, received almost 300 millimeters (1 foot) of rain more than normal.
The initial effects of La Niña were to cool surface waters in the eastern Pacific Ocean and push moisture to the west. A climate pattern known as the Southern Annular Mode then coaxed the moisture into Australia’s interior, causing widespread flooding across the continent. Later in the event, high levels of moisture from the Indian Ocean driven by the Indian Ocean Dipole collided with La Niña-borne moisture in the Pacific and pushed even more moisture into the continent’s interior. Together, these influences spurred one of the wettest periods in Australia’s recorded history.
Australia’s vast interior, called the Outback, is ringed by coastal mountains and often quite dry. Because of the low-lying nature of the continent’s eastern interior and the lack of river runoff in its western dry environment, most of the heavy rainfall of 2010–11 remained inland rather than flowing into the oceans. While some of it evaporated in the desert sun, much of it sank into the dry, granular soil of the Western Plateau or filled the Lake Eyre basin in the east.
“No other continent has this combination of atmospheric set-up and topography,” Fasullo says. “Only in Australia could the atmosphere carry such heavy tropical rains to such a large area, only to have those rains fail to make their way to the ocean.”
Measuring the difference
To conduct the research, the scientists turned to three cutting-edge observing instrument systems:
- NASA’s Gravity Recovery and Climate Experiment (GRACE) satellites, which make detailed measurements of Earth’s gravity field. The satellites enable scientists to monitor changes in the mass of continents.
- The Argo global array of 3,000 free-drifting floats that measure the temperature and salinity of the upper 6,000 feet of the world’s oceans.
- Satellite-based altimeters that are continuously calibrated against a network of tide gauges. Scientists subtract seasonal and other variations to closely estimate global sea level changes.
Using these instruments, the researchers found that the mass in Australia and, to a lesser extent, South America began to increase in 2010 as the continents experienced heavy and persistent rain. At the same time, sea levels began to measurably drop.
Since 2011, when the atmospheric patterns shifted out of their unusual combination, sea levels have been rising at a faster pace of about 10 millimeters (0.4 inches) per year.
Scientists are uncertain how often the three atmospheric events come together to cause such heavy rains over Australia. Fasullo believes there may have been a similar event in 1973-74, which was another time of record flooding in that continent. But modern observing instruments did not exist then, making it impossible to determine what took place in the atmosphere and whether it affected sea level rise.
“Luckily we’ve got great observations now,” Fasullo says. “We need to maintain these observing platforms to understand what is a complicated climate system.”
The study was funded by the National Science Foundation, which is NCAR’s sponsor, and by NASA.
The work was published today in Geophysical Research Letters, a journal of the American Geophysical Union.
Mary Catherine Adams
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Bob Henson, NCAR/UCAR Media Relations
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David Hosansky, NCAR/UCAR Media Relations
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Journalists can download a PDF copy of this accepted article by clicking on this link:
Neither the paper nor this press release is under embargo.
“Australia's unique influence on global sea level in 2010–2011”
John T. Fasullo: National Center for Atmospheric Research, Boulder, CO;
Carmen Boening and Felix W. Landerer: Jet Propulsion Laboratory, California Institute of Technology, Pasadena, CA, USA;
R. Steven Nerem: Colorado Center for Astrodynamics Research, University of Colorado at Boulder, Boulder, CO.
Contact information for the authors:
John Fasullo, Telephone: +1 (303) 497-1712, Email: [email protected]