Critical data from space aids lake ice research
The Canadian Space Agency launched a trio of satellites on June 12 and University of Toronto Mississauga cryospheric scientist Laura Brown says this is great news. The RADARSAT Constellation Mission (RCM) provides satellite and radar images of all of Canada’s territory daily, as well as images of the Arctic up to four times a day.
“Thanks to the new RADARSAT Constellation Mission, there will be much better coverage so we won’t have gaps in the data,” says Brown, an associate professor in the Department of Geography.
Brown studies lake ice in both the Arctic and temperate regions. She wants to know how fresh water ice and snow are responding to the change in climate. She combines the satellite data with information from other sources to represent the ice and snow system in climate models.
Until now, Brown accessed data from the RCM’s predecessor. “But my field site in Haliburton is just outside the region with daily coverage by RADARSAT-2, so we only had imagery about one in every three days from the radar bands we need,” she says. She and her research team filled the data gaps by inferring it through temperature data. “But actually being able to visualize the ice cover itself, is so much better than just looking at the temperature.”
Climate by proxy
Brown says that lake ice is a proxy of our climate. “If the climate warms or cools, if there is a change in the snow, the ice responds.”
Temperate region lake ice differs from arctic ice. Arctic ice is thick and black with just a thin layer of white reflective ice from snow on top. Arctic ice stays frozen until spring. In temperate regions, snow piles up on lake ice, mid-winter thaws cause flooding, then the water refreezes. “So we get a layer of white ice which is more reflective but thinner ice overall and not as strong,” Brown says.
With more data from the RCM, Brown will be able to see daily surface changes from mid-winter thaws and track how often they happen. She will be able to develop models to better project if lake ice is forming later and disappearing sooner.
“We also use the satellites to look at a larger area from space. Rather than just drill a hole and look at one lake, we can look at a whole region at once to see how it is changing,” she says.
Above and below the lake ice
A change in ice cover impacts recreational activities on the ice like snowmobiling and ice fishing. It impacts transportation over ice roads. It also impacts what happens under the ice.
Brown says that less ice cover means more open water. More open water means more evaporation and more sunlight coming into the lake. “This would change the organisms living in the lake that respond to different light conditions. It could also change the nutrients within the lake,” says Brown.
In a forthcoming paper, Brown and PhD candidate Alexis Robinson have developed a new climate model “to better represent the reflectivity of our ice cover here so that we can get the melt timing with more accuracy.”
Brown, members of her research team and a scientist from her industry partner Campbell Scientific Canada are preparing to travel to the Arctic for two weeks at the end of July.
They will live and work out of the Polar Continental Shelf Program’s research station in Resolute, an Inuit community, on Cornwallis Island in Nunavut. With help from a member of the Resolute Bay Hunters and Trappers Association, Brown will collect data on arctic lake ice conditions from two of her research lakes.
Then the researchers will fly to Polar Bear Pass National Wildlife Area on Bathurst Island where Brown has another lake instrumented to observe ice cover. She also helps to maintain Campbell Scientific’s weather tower there in exchange for data.
Learning to live with climate change
“By the end of the century, the research lakes in Haliburton probably won't have ice cover every year,” says Brown. “Our research will help Canadians and others in temperate regions around the world as we learn to live with our changing climate.”