Glaciologist using 3D models to study loss of shelf ice at Milne Fjord

The partial collapse of the Milne Fjord ice shelf has become a key focus of Arctic researchers, from oceanographers to glaciologists.

By Madalyn Howitt, Nunatsiaq News - August 24, 2022
Glacier researcher Anna Crawford (left) pulls a device that is collecting data on the thickness of the Milne Fjord ice shelf on a research trip to Ellesmere Island earlier this month. Crawford uses 3D computer models to look at how glaciers and different forms of big ice deteriorate. (Dustin Patar)

Until recently, Ellesmere Island’s Milne Fjord was home to one of only a few known epishelf lakes — freshwater lakes that form when water runoff from land becomes trapped in a fjord behind a floating ice shelf — in the Arctic.

That floating ice shelf — known as the Milne Fjord ice shelf — partially collapsed in July 2020, causing the lake to drain. The aftermath of that event has since become a key focus of Arctic researchers, from oceanographers to glaciologists.

One of those researchers is ice shelf expert Anna Crawford, a postdoctorate fellow at the University of Edinburgh and a recent recipient of a $25,000 Trebek Initiative grant, named after the late Jeopardy! host Alex Trebek.

The initiative, a joint venture between the National Geographic Society and the Royal Canadian Geographical Society, provides grants to emerging educators, conservationists, researchers and others who are documenting Canadian and Indigenous land, wildlife, water, culture and history.

Crawford used the grant to travel earlier this month as part of an eight-person team to Milne Fjord, where she surveyed the ice shelf to collect data that will help quantify the impact of sea-ice loss on the ice shelf’s stability.

She uses 3D computer models to look at how glaciers and different forms of ice deteriorate, allowing her to simulate the processes that glaciers or ice shelves go through.

An aerial view of the Milne Fjord ice shelf. (Anna Crawford)

“Glaciers aren’t static, they flow and then they also break and it produces icebergs, so these 3D models allow me to build a computer representation of a glacier and then let me kind of evolve it and see how it behaves,” Crawford said.

“I can apply different conditions. I can make it slow, faster, or I could make it warmer, or I could make the environment around the glacier warmer. I can then use those simulations with the software program to see how the glacier reacts to those different factors.”

To collect the data, Crawford used an ice-penetrating radar while she walked along the surface of the ice shelf. Milne Fjord’s ice shelf is a perennial ice feature about 100 meters (or 328 feet) thick, so it “doesn’t drift away or reform every year. It’s been there for a long time,” she said.

She also spent time doing an aerial photo survey with help from a helicopter when weather conditions permitted it.

She was able to collect a three-kilometer stretch of ice-thickness data that will help show how the epishelf lake drained two years ago, and act as baseline data from which researchers can monitor glacial change.

The epishelf lake is important, said Crawford, because it’s “like a bottomless freshwater lake and instead of the bottom being ground, the bottom is the salt water from the ocean,” allowing for a “really unique biological ecosystem to exist.”

Anna Crawford (center) takes a break with her research with teammates Derek Mueller (left) and Erik Wagenaar on a trip to study the Milne Fjord ice shelf at Ellesmere Island earlier this month. (Cameron Fitzpatrick)

The Milne Fjord epishelf lake was the last known epishelf lake in the Canadian Arctic, and there may only be a few others in other Arctic regions, Crawford said.

Several epishelf lakes once existed along the northern coast of Ellesmere Island, but the gradual thinning and break-up of ice shelves from climate change has resulted in drainage events and the loss of most of these lakes. Researchers observed that in July 2020, the Milne Fjord ice shelf lost 40 percent of its surface area.

“That’s been kind of disheartening from one angle, but also very interesting,” Crawford said of the loss of the epishelf lake at Milne Fjord.

“Now we have a natural laboratory to keep returning to study the impact of that lake drainage on the remaining elements of that fjord system.”

Ultimately, Crawford is interested in using her 3D models to study how the ice shelf is made more vulnerable by the loss of sea ice that can provide some protection to the more permanent ice shelves.

Also, she wants to examine the way the stability of ice shelves could be affected if more sea ice is lost, which scientists anticipate will happen due to climate change.

By visiting Milne Fjord in person, Crawford was able to “slingshot” her research in this area, she said.

“A lot of times, us in the glacier modeling community don’t actually get to travel to the sites that we’re simulating and studying, but it’s really valuable if we can do those visits because it gives us that eyes on the ground and a chance to better understand the major factors at play in such a system,” she said.

“Those are the factors that really need to be represented accurately when we go and do these simulations with our computer models.”