New research reveals how a climate model commonly used by geoscientists currently overestimates a key physical property of Earth’s climate system called albedo.
Albedo is the degree to which ice reflects planet-warming sunlight into space.
As the planet continues to warm due to human-driven climate change, accurate computer climate models will be key in helping illuminate exactly how the climate will continue to be altered in the years ahead.
“We found that with old model versions, the ice is too reflective by about 5%,” says Chloe Clarke, a project scientist in University of California, Irvine professor Charlie Zender’s group. “Ice reflectivity was much too high.”
The amount of sunlight the planet receives and reflects is important for estimating just how much the planet will warm in the coming years. Previous versions of the model, called the Energy Exascale Earth System Model (E3SM), overestimated albedo because they did not account for what Clarke described as the microphysical properties of ice in a warming world.
Those properties include the effects things like algae and dust have on albedo. Dark-colored algae and dust can make snow and ice less reflective and less able to reflect sunlight.
To do the analysis, Clarke and her team studied satellite data to track the albedo of the Greenland Ice Sheet. They found that E3SM reflectivity overestimates the reflectivity of the ice sheet, “meaning the model estimates less melt than what would be expected from the ice microphysical properties,” says Clarke.
But with the new ice reflectivity incorporated into the model, the Greenland Ice Sheet is melting at a rate of about six gigatons more than in older model versions. This is based on albedo measurements that are more consistent with satellite observations.
Clarke hopes her team’s study stresses the importance of the seemingly minuscule properties that can have far-reaching consequences for the overall climate.
“I think our work is going to help models do a much better job of helping us capture snow and ice-related climate feedbacks,” she says.
Next, Clarke wants to study different icy parts of the planet to gauge how widespread the albedo discrepancy is in E3SM.
“Our next steps are to get it so it is functional globally and not just valid over Greenland,” says Clarke, who also intends to compare the new Greenland Ice Sheet melt rates to observations to measure how much more accurate the new ice albedo is.
“It would be useful to apply it to glaciers in places like the Andes and Alaska.”
The study appears in the Journal of Geophysical Research: Atmospheres.
Additional authors are from Lamont-Doherty Earth Observatory, University of Michigan, National Oceanic and Atmospheric Administration, and UC Irvine.
Funding information is listed in the study.
Source: UC Irvine
