NASA-MIT study evaluates efficiency of oceans as heat sink, atmospheric gases sponge
Credit: NASA’s Goddard Space Flight Center.
By Ellen Gray,
NASA’s Goddard Space Flight Center
The world’s oceans are like brakes slowing down the full effects of greenhouse gas warming of the atmosphere. Over the last ten years, one-fourth of human-emissions of carbon dioxide as well as 90 percent of additional warming due to the greenhouse effect have been absorbed by the oceans. Acting like a massive sponge, the oceans pull from the atmosphere heat, carbon dioxide and other gases, such as chlorofluorocarbons, oxygen and nitrogen and store them in their depths for decades to centuries and millennia.
New NASA research is one of the first studies to estimate how much and how quickly the ocean absorbs atmospheric gases and contrast it with the efficiency of heat absorption. Using two computer models that simulate the ocean, NASA and MIT scientists found that gases are more easily absorbed over time than heat energy. In addition, they found that in scenarios where the ocean current slows down due to the addition of heat, the ocean absorbs less of both atmospheric gases and heat, though its ability to absorb heat is more greatly reduced. The results were published in Geophysical Research Letters, a journal of the American Geophysical Union.
“As the ocean slows down, it will keep uptaking gases like carbon dioxide more efficiently, much more than it will keep uptaking heat. It will have a different behavior for chemistry than it has for temperature,” said Anastasia Romanou, lead author and climate scientist at NASA’s Goddard Institute for Space Studies and Columbia University in New York City.
Credit: NASA’s Goddard Space Flight Center.
She and colleagues at the Massachusetts Institute of Technology in Cambridge, Massachusetts used the NASA GISS ocean model and the MIT General Circulation Model to simulate one of the Atlantic’s major current systems that delivers absorbed heat and gases to the depths.
In the Atlantic Ocean, the Gulf Stream is part of what’s called the Atlantic Meridional Overturning Circulation, a conveyor belt of ocean water that carries warm water from Florida to Greenland where it cools and sinks to 1000 meters (about 3281 feet) or more before traveling back down the coast to the tropics. On its northward journey, the water at the surface absorbs gases like carbon dioxide and chlorofluorocarbons (CFCs) – the latter are, to a large extent, the gases responsible for the ozone hole over Antarctica – as well as excess heat from the atmosphere. When it sinks near Greenland, those dissolved gases and heat energy are effectively buried in the ocean for years to decades and longer. Removed from the atmosphere by the ocean, the impact of their warming on the climate has been dramatically reduced.
To understand and quantify the ocean’s sponge-like capabilities, the researchers used the two independent models of Atlantic Ocean currents together with shipboard observations of chlorofluorocarbons as a starting point. Chlorofluorocarbons are what’s called a passive tracer.
The red line on the map shows the Gulf Stream current, the surface portion of the Atlantic Meridional Overturning Circulation. Shown in shades of blue are the concentrations of CFCs at depth in the ocean. Nearer to the equator, the CFCs only occur at the surface. As the Gulf Stream current moves north, they begin to be drawn down to depth with the downward pull of the conveyor belt. Image credit: NASA/Jenny Hottle.
“I think of it as a colored dye,” said co-author John Marshall, a professor of oceanography at the Massachusetts Institute of Technology. “If I have a bucket of water and just stir it around and put some food coloring in it, the dye goes down into the water, and it doesn’t influence the circulation of the water.”
In the real world as well as in the model, this allows scientists to “see” how much of the gas is absorbed from the atmosphere into the ocean and then follow it as it travels around the world in the currents. Adding heat to the ocean, in contrast, slows down the overturning circulation because ocean currents depend on temperature gradients – moving from warmer locations to cooler locations – that weaken under global warming as cooler waters heat up. This means that estimating how much heat the ocean absorbs by only using a tracer may not be accurate.
“The results show that we need to think differently about how the ocean responds to taking up heat and passive tracers or greenhouse gases. Then we need to study them in parallel but using different methods,” Romanou said.
These results from the computer models of the Atlantic Meridional Overturning Circulation are one of the many moving parts that come together in global climate models. By refining scientists’ understanding of how efficiently gases and heat are taken up, the finding will improve global climate model projections for future climate scenarios, said Marshall. This is especially true for projections that stretch tens or a hundred years into the future, when those tracers and other gases that behave similarly like carbon dioxide, as well as excess heat energy, reach the upward turn of the conveyor belt and return to the surface. When that happens some portion of them will return to the atmosphere after their long underwater journey around the planet.
“Most of the excess heat from climate change will go into the ocean eventually, we think,” Romanou said. “Most of the excess chemical pollutants and greenhouse gases will be buried in the ocean. But the truth is that the ocean recirculates that extra load and, at some point, will release some of it back to the atmosphere, where it will keep raising temperatures, even if future carbon dioxide emissions were to be much lower than they are now.”
This eventual release of buried gases and heat from the oceans is sometimes called the “warming in the pipeline” or “warming commitment” that people will eventually have to contend with, Romanou said.
Romanou, A., J. Marshall, M. Kelley, and J. Scott, 2017: Role of the ocean’s AMOC in setting the uptake efficiency of transient tracers. Geophys. Res. Lett., early on-line, doi:10.1002/2017gl072972.
Leslie McCarthy, NASA Goddard Institute for Space Studies, New York, N.Y., 212-678-5507, email@example.com
Michael Cabbage, NASA Goddard Institute for Space Studies, New York, N.Y., 212-678-5516, firstname.lastname@example.org