How coastal ocean currents increase Antarctic ice shelf melt.
A new model suggests that Antarctica’s ice shelves may be melting at an accelerated rate, which could eventually contribute to more rapid sea level rise. The model accounts for an often-overlooked narrow ocean current along the Antarctic coast. It simulates how rapidly flowing freshwater, melted from the ice shelves, can trap dense warm ocean water at the base of the ice, causing it to warm and melt even more.
The new model was developed by researchers at the California Institute of Technology (Caltech) and Jet Propulsion Laboratory (JPL). Recently published in the journal Science Advances, the study was conducted in the laboratory of Andy Thompson, professor of environmental science and engineering.
Ice shelves are outcroppings of the Antarctic ice sheet, found where the ice juts out from land and floats on top of the ocean. The shelves, which are each several hundred meters thick, act as a protective buffer for the mainland ice, keeping the whole ice sheet from flowing into the ocean (which would dramatically raise global sea levels). However, the speed at which these ice shelves are melting is increasing due to a warming atmosphere and warming oceans caused by climate change. This is threatening their ability to hold back the flow of the ice sheet into the ocean.
“If this mechanism that we’ve been studying is active in the real world, it may mean that ice shelf melt rates are 20 to 40 percent higher than the predictions in global climate models, which typically cannot simulate these strong currents near the Antarctic coast,” Thompson says.
Led by senior research scientist Mar Flexas, the researchers in this study focused on one area of Antarctica: the West Antarctic Peninsula (WAP). Antarctica is roughly shaped like a disk, except where the WAP protrudes out of the high polar latitudes and into lower, warmer latitudes. It is here that Antarctica sees the most dramatic changes due to climate change. The team has previously deployed autonomous vehicles in this region, and scientists have used data from instrumented elephant seals to measure temperature and salinity in the water and ice.
The team’s model takes into account the narrow Antarctic Coastal Current that runs counterclockwise around the entire Antarctic continent. Because it is so small, this is a current that many climate models do not include.
“Large global climate models don’t include this coastal current, because it’s very narrow—only about 20 kilometers wide, while most climate models only capture currents that are 100 kilometers across or larger,” Flexas explains. “So, there is a potential for those models to not represent future melt rates very accurately.”
The model illustrates how freshwater that melts from ice at the WAP is carried by the coastal current and transported around the continent. The less-dense freshwater moves along quickly near the surface of the ocean and traps relatively warm ocean saltwater against the underside of the ice shelves. This then causes the ice shelves to melt from below. In this way, increased meltwater at the WAP can propagate climate warming via the Coastal Current, which in turn can also escalate melting even at West Antarctic ice shelves thousands of kilometers away from the peninsula. This remote warming mechanism may be part of the reason that the loss of volume from West Antarctic ice shelves has accelerated in recent decades.
“There are aspects of the climate system that we are still discovering,” Thompson says. “As we’ve made progress in our ability to model interactions between the ocean, ice shelves, and atmosphere, we’re able to make more accurate predictions with better constraints on uncertainty. We may need to revisit some of the predictions of sea level rise in the next decades or century—that’s work that we’ll do going forward.”
Reference: “Antarctic Peninsula warming triggers enhanced basal melt rates throughout West Antarctica” by M. Mar Flexas, Andrew F. Thompson, Michael P. Schodlok, Hong Zhang and Kevin Speer, 12 August 2022, Science.
In addition to Flexas and Thompson, additional coauthors are Michael Schodlok and Hong Zhang of JPL, and Kevin Speer of Florida State University. Funding was provided by the National Science Foundation, the NASA Physical Oceanography program and Cryospheric Sciences program, NASA’s Internal Research and Technology Development program (Earth 2050 project), JPL, and Caltech. Caltech manages JPL for NASA.