Geoengineering may slow Greenland ice sheet loss

Peer-Reviewed Publication

HOKKAIDO UNIVERSITY

 

IMAGE: 

RESULTS OF THE SICOPOLIS SIMULATIONS COMPARING THE CHANGE OF THE GREENLAND ICE SHEET BETWEEN GEOMIP G4 AND RCP4.5: ICE THICKNESS (H). STRATOSPHERIC AEROSOL INJECTION OF SULFUR DIOXIDE WILL HAVE THE GREATEST PROTECTIVE EFFECT ON THE MARGINS (WHICH REMAIN THICKER; YELLOW AND RED) OF THE ICE SHEET. (JOHN C. MOORE, RALF GREVE ET AL. JOURNAL OF GEOPHYSICAL RESEARCH: EARTH SURFACE. NOVEMBER 27, 2023)

view more 

CREDIT: JOHN C. MOORE, RALF GREVE ET AL. JOURNAL OF GEOPHYSICAL RESEARCH: EARTH SURFACE. NOVEMBER 27, 2023

Modeling shows that stratospheric aerosol injection has the potential to reduce ice sheet loss due to climate change.

One of the many effects of global warming is sea-level rise due to the melting and retreat of the Earth’s ice sheets and glaciers as well as other sources. As the sea level rises, large areas of densely populated coastal land could ultimately become uninhabitable without extensive coastal modification. In order to stave off this possibility, carbon emissions need to reach net negative, a state that is hard to achieve under current circumstances.

There are many proposals to drastically mitigate the effects of climate change, and the most expansive of these involve interventions that will alter aspects of the entire globe—the geoengineering techniques. While they have some promise, we do not understand enough about natural cycles to fully assess how beneficial such interventions will be.

An international team of researchers led by Professor John C. Moore, at the University of Lapland, Rovaniemi, Finland, and Professor Ralf Greve, at the Institute of Low Temperature Sciences, Hokkaido University, has used simulations to examine the potential effects of a geoengineering technique called stratospheric aerosol injection on ice sheet melting. Their findings were published in the Journal of Geophysical Research: Earth Surface.

“Stratospheric aerosol injection, or SAI, would artificially introduce aerosols into the stratosphere by aircraft or high-altitude balloons to create a cooling effect via global dimming and increased albedo—the degree to which Earth reflects sunlight,” Moore explains.

Moore, Greve and colleagues used the SICOPOLIS model to simulate the changes in the Greenland Ice Sheet for the period 1990–2090 under three different scenarios: RCP8.5 (worst-case scenario, unabated warming); RCP4.5 (intermediate scenario, possibly achievable under current conditions); and GeoMIP G4 (RCP4.5 plus the injection of 5 million metric tons of sulfur dioxide per year into the stratosphere during 2020–2070).

The simulations showed that SAI of sulfur dioxide would have a clear protective effect on the Greenland Ice Sheet. Under RCP8.5, there would be ice loss equivalent to approximately 90 mm sea-level rise; under RCP4.5, ice loss would be approximately 60.6 mm sea-level rise; but under GeoMIP G4, ice loss would be limited to approximately just 37.6 mm sea-level rise. When these scenarios were tested with a different model, Elmer/Ice, the results were similar. The margins of the ice sheet would benefit the most under GeoMIP G4.

“While this study shows that SAI could contribute to the protection of the Greenland Ice Sheet, and hence, potentially, all other ice cover on Earth, geoengineering is a highly contentious topic,” Greve concludes. “The biggest issue is that it addresses only the symptoms of global warming, not the root causes—and may even delay the changes required to address the causes. Furthermore, due to the immense complexity of the natural systems on Earth, it is impossible to predict exactly what positive and negative outcomes could result.”

 

Simulated mass loss of the Greenland ice sheet from 1990 until 2090, expressed as a sea-level contribution, under different conditions:RCP8.5 (red; worst-case scenario, unabated warming), RCP4.5 (green; intermediate scenario, possibly achievable under current conditions), and GeoMIP G4 (blue; RCP4.5 plus the injection of 5 million metric tons of sulfur dioxide per year into the stratosphere during 2020–2070). (Ralf Greve)

CREDIT

Ralf Greve

JOURNAL

Journal of Geophysical Research Earth Surface

DOI

10.1029/2023JF007112 

METHOD OF RESEARCH

Computational simulation/modeling

SUBJECT OF RESEARCH

Not applicable

ARTICLE TITLE

Reduced Ice Loss From Greenland Under Stratospheric Aerosol Injection