From the National Science Foundation

Oceanographers, marine biologists and geologists are the scientists most commonly associated with studying changes in sea ice. But these days, it just might be a mathematician drilling ice cores in the Antarctic.

With 17 trips to the Arctic and Antarctic under his belt, Ken Golden of the University of Utah has made a career of helping better understand the mathematics of what goes on inside the thick layers of sea in those regions.

Understanding sea ice and how it behaves could advance research across a wide range of sciences. For instance, it could help scientists predict how fast sea ice will melt, the impact of shrinking polar ice caps on Earth’s climate system, or lead to better composite materials based on the structure of sea ice. And that’s just the beginning.

 

“Sea ice is a very complicated system,” says Golden, who has been studying it firsthand since his first expedition to Antarctica in 1980. “When you go down there, you see how it interacts with the ocean, how it interacts with the waves, with the atmosphere.”

These interactions between sea ice and its environment change the ice and how it behaves. That’s because sea ice, although it appears to be solid, is actually a composite material, made up of more than one ingredient.

Columnar sea ice, which is more common in the Arctic, is composed of vertically-oriented, pure ice crystals jammed into uncomfortably close quarters, with tiny pockets of brine filling out the sub-millimeter nooks and crannies. Granular sea ice, more commonly found in the Antarctic, is finer and more granular in structure, but is similarly composed of ice crystals and brine.

With support from the National Science Foundation (NSF), Golden has been studying composite materials and sea ice structure since 1984, when he was an NSF Mathematical Sciences postdoctoral fellow at Rutgers. He says the lessons researchers learn from the structure and behavior of sea ice can lead to a better understanding of high-tech or biologically-important composite materials. For example, he said, “how to monitor osteoporosis in human bone, which turns out to be extremely close in structure to sea ice.”

A rubber-suited Ken Golden wades into icy Arctic waters to measure the depth of this melt pond. Understanding how environmental conditions like temperature and incoming solar radiation affect percolation, or the movement of water up and down through sea ice, could help scientists better predict how sea ice might respond to changes in its environment.

PHOTO CREDIT: Don Perovich

A rubber-suited Ken Golden wades into icy Arctic waters to measure the depth of this melt pond. Understanding how environmental conditions like temperature and incoming solar radiation affect percolation, or the movement of water up and down through sea ice, could help scientists better predict how sea ice might respond to changes in its environment.

Victor Roytburd, director of the NSF Division of Mathematical Sciences, calls Golden’s work “a textbook example of the application of mathematics to understanding complex natural phenomena.”

The basic physical laws that govern the “life of ice” in Golden’s work are fairly clear, but understanding the intricate interactions between sea ice and its environment requires penetrating research into the hierarchy of those phenomena, Roytburd said.

“Taking into account the role that mathematics plays as a universal language unifying natural sciences, it is not surprising that mathematics and its applications play so important and fundamental role in so many disciplines,” he said. “Ken Golden’s work contributes invaluable insights to understanding and perhaps managing life and evolution of sea ice.”

The life inside and outside sea ice

Ask Golden to sum up the most fascinating thing about sea ice and he replies: Percolation–the movement of water up and down through the complex microstructure of the ice. Percolation, he says, is essential for the ice pack’s health.

Researchers believe almost 25 percent of the ice in Antarctica is created when water floods the surface. Much of that water comes up through the porous microstructure of the underlying ice, and freezes into what’s called “snow-ice.”

Percolation also brings vital nutrients up from the ocean, helping sustain algae that live within the brine inside the ice. Algae inside sea ice might sound isolated from the larger marine ecosystem, but that isn’t the case.

A thin crust of snow hides sea ice in various stages of melting and re-freezing. Sea ice temperature and salinity are critical to determining whether or not percolation will occur.

PHOTO CREDIT: Ken Golden, University of Utah

A thin crust of snow hides sea ice in various stages of melting and re-freezing. Sea ice temperature and salinity are critical to determining whether or not percolation will occur.

Columbia University marine ecologist Craig Aumack researches how algae living in the sea ice off the coast of Barrow, Alaska, connect to the surrounding marine ecosystem. Algae start to bloom when temperatures warm in spring, he says.

“Then, as the snow completely melts and they start getting lots and lots of light, they migrate down to the bottom of the ice and eventually leave the ice into the water column.”

That’s where they become food for algae-eaters that, in turn, contribute to the larger food cycle in the ocean.

Ice-dwelling algae have carved out a precarious existence inside sea ice, relying on percolation for food. But whether or not fluid percolates through the ice depends on a delicate balance of temperature and salinity within the ice itself. Tilt the balance this way or that, and percolation does not occur.

The risks of mathematical field research

Field research on sea ice has proved riskier than other types of data collection. Golden and his colleagues have faced natural threats, ranging from life-threatening cracks in sea ice to equipment issues.

In 1998, Golden was on the Australian ice breaker Aurora Australis, about 12 hours into a journey inside Antarctica’s ice edge, when a fire alarm went off. There was a fire in the engine room and the flames were out of control. The nearest help was hours away, with nothing for miles but water and ice.

“You’re down there”, Golden says, “and you’re on your own.”

It took a few nerve-wracking hours, but the crew finally controlled the fire with no injuries.

“We were basically there for five days,” Golden says. “First two days with no power, no toilets or anything like that.”

Pathways through sea ice. Ice core taken from Arctic sea ice shows where brine pockets have connected to form channels, with a distinctly visible pathway in the middle. Channels and pathways like these allow sea water or fresh melt water to move, or percolate, through the sea ice.

PHOTO CREDIT: Ken Golden, University of Utah

Pathways through sea ice. Ice core taken from Arctic sea ice shows where brine pockets have connected to form channels, with a distinctly visible pathway in the middle. Channels and pathways like these allow sea water or fresh melt water to move, or percolate, through the sea ice.

Sharing his explorer spirit

At the university, Golden works with students enthralled with polar ice and the scientific questions it poses.

His work, from demonstrating a meter-long ice-core drill to organizing research trips to the polar regions, attracts students from across disciplines including mechanical engineering, bioengineering, electrical engineering, physics and chemistry. The study of sea ice, Golden says, sits at the nexus of many different areas of study.

“I think ultimately what we’d really love to do is to bring more people into mathematics and show how mathematics is really the operating system of science and engineering,” he says.

Investigators
Kenneth Golden

Related Institutions/Organizations
University of Utah

The albedo effect: Networks of melt ponds create darker areas on the otherwise-reflective surface of sea ice. The result? Whereas the white surface of the sea ice reflects solar radiation, the darker melt ponds absorb it. More advanced models of the evolution of melt ponds over the polar summer could help researchers improve long term projections of sea ice melt, and better understand the role of sea ice in Earth's climate system.

PHOTO CREDIT: Don Perovich

The albedo effect: Networks of melt ponds create darker areas on the otherwise-reflective surface of sea ice. The result? Whereas the white surface of the sea ice reflects solar radiation, the darker melt ponds absorb it. More advanced models of the evolution of melt ponds over the polar summer could help researchers improve long term projections of sea ice melt, and better understand the role of sea ice in Earth’s climate system.

Related Programs
Applied Mathematics
Arctic Natural Sciences
Mathematical Sciences Infrastructure Program

Related Awards
#1413454 Homogenization for Sea Ice
#0940249 Collaborative Research: Mathematics and Climate Change Research Network

Total Grants
$847,727

Related Websites
Ken Golden website, University of Utah: http://www.math.utah.edu/~golden/

 

Media Contacts

Ken Goldenprofessor of mathematics
Mobile: 801-750-8555

Amina KhanNational Science Foundation
Office: 703-292-8791

Lee Siegelsenior science writer, University of Utah Communications (Note: I have retired from the university. Please contact the communications office at 801-585-9244. Please note new personal phone number; my university extension and cell have been disconnected.)
Mobile: 801-272-3331