Robotic ocean gliders are offering clues as to how warm water is making its way to Antarctic ice sheets—and how the warming ultimately leads to rising ocean levels.
The rapidly melting ice sheets on the coast of West Antarctica are a potential major contributor to rising ocean levels worldwide. Although warm water near the coast is thought to be the main factor causing the ice to melt, the process by which this water ends up near the cold continent is not well understood.
The gliders show that swirling ocean eddies, similar to atmospheric storms, play an important role in transporting warm waters to the Antarctic coast—a discovery that scientists say will help determine how rapidly the ice is melting and, as a result, how quickly ocean levels will rise.
“When you have a melting slab of ice, it can either melt from above because the atmosphere is getting warmer or it can melt from below because the ocean is warm,” says lead author Andrew Thompson, assistant professor of environmental science and engineering at California Institute of Technology (Caltech).
“All of our evidence points to ocean warming as the most important factor affecting these ice shelves, so we wanted to understand the physics of how the heat gets there.”
Ordinarily when oceanographers like Thompson want to investigate such questions, they use ships to lower instruments through the water or they collect ocean temperature data from above with satellites, but these techniques are problematic in the Southern Ocean.
“Observationally, it’s a very hard place to get to with ships. Also, the warm water is not at the surface, making satellite observations ineffective,” Thompson says.
Gliders ‘phone home’
Because the gliders are small—only about six feet long—and are very energy efficient, they can sample the ocean for much longer periods than large ships can. When the glider surfaces every few hours, it “calls” the researchers via a mobile phone–like device located on the tail, allowing the researchers to almost immediately access the information the glider has collected.
Like airborne gliders, the bullet-shaped ocean gliders have no propeller; instead they use batteries to power a pump that changes the glider’s buoyancy. When the pump pushes fluid into a compartment inside the glider, the glider becomes denser than seawater and less buoyant, thus causing it to sink.
If the fluid is pumped instead into a bladder on the outside of the glider, the glider becomes less dense than seawater—and therefore more buoyant—ultimately rising to the surface. Like airborne gliders, wings convert this vertical lift into horizontal motion.
For the new study, published in the journal Nature Geoscience, Thompson and colleagues from the University of East Anglia dropped the gliders into the ocean off the coast of the Antarctic Peninsula in January 2012. The robotic vehicles then spent the next two months moving up and down through the water column—diving a kilometer below the surface of the water and back up again every few hours—exploring the Weddell Sea off the coast of Antarctica.
As the gliders traveled, they collected temperature and salinity data at different locations and depths of the sea.
The glider’s up and down capability is important for studying ocean stratification, or how water characteristics, such as density, change with depth, Thompson says.
“If it was only temperature that determined density, you’d always have warm water at the top and cold water at the bottom. But in the ocean you also have to factor in salinity; the higher the salinity is in the water, the more dense that water is and the more likely it is to sink to the bottom,” he says.
Warm water sandwich
In Antarctica the combined effects of temperature and salinity create an interesting situation, in which the warmest water is not on top, but actually sandwiched in the middle layers of the water column.
“That’s an additional problem in understanding the heat transport in this region,” Thompson says. You can’t just take measurements at the surface. “You actually need to be taking a look at that very warm temperature layer, which happens to sit in the middle of the water column. That’s the layer that is actually moving toward the ice shelf.”
The gliders reveal that the heat was actually coming from a less predictable source: eddies, swirling underwater storms that are caused by ocean currents.
“Eddies are instabilities that are caused by ocean currents, and we often compare their effect on the ocean to putting a spoon in your coffee,” Thompson says. “If you pour milk in your coffee and then you stir it with a spoon, the spoon enhances your ability to mix the milk into the coffee and that is what these eddies do. They are very good at mixing heat and other properties.”
Eddies in action
Because the gliders could dive and surface every few hours and remain at sea for months, they were able to see these eddies in action—something that ships and satellites had previously been unable to capture.
“Ocean currents are variable, and so if you go just one time, what you measure might not be what the current looks like a day later. It’s sort of like the weather—you know it’s going to be warm in the summer and cold in the winter, but on a day-to-day basis it could be cold in the summer just because a storm came in,” Thompson says.
“Eddies do the same thing in the ocean, so unless you understand how the temperature of currents is changing from day to day—information we can actually collect with the gliders—then you can’t understand what the long-term heat transport is.”
In future work, Thompson plans to couple meteorological data with the data collected from his gliders. In December, the team will use ocean gliders to study a rough patch of ocean between the southern tip of South America and Antarctica, called the Drake Passage, as a surface robot, called a Waveglider, collects information from the surface of the water.
“With the Waveglider, we can measure not just the ocean properties, but atmospheric properties as well, such as wind speed and wind direction. So we’ll get to actually see what’s happening at the air-sea interface.”
In the Drake Passage, deep waters from the Southern Ocean are “ventilated”—or emerge at the surface—a phenomenon specific to this region of the ocean. That makes the location important for understanding the exchange of carbon dioxide between the atmosphere and the ocean.
“The Southern Ocean is the window through which deep waters can actually come up to ‘see’ the atmosphere”—and it’s also a window for oceanographers to more easily see the deep ocean,” he says. “It’s a very special place for many reasons.”
Andrew Stewart, a former postdoctoral scholar at Caltech who is now at UCLA, and researchers at the University of East Anglia and at GEOMAR Helmholtz Centre for Ocean Research-Kiel are coauthors of the study.
The National Science Foundation and the UK’s Natural Environment Research Council provided funding.