Use of fossil fuels will see more than 40% of glacial mass disappear by 2100, warns study

LinkedIn +

A new international study led by Carnegie Mellon University (CMU) in Pittsburgh, Pennsylvania shows that the world could lose as much as 41% of its total glacier mass this century, or as little as 26%, depending on immediate climate change mitigation efforts.

The international team produced new projections of glacier mass loss through the century under different emissions scenarios. The projections were aggregated into global temperature-change scenarios to support adaptation and mitigation discussions, such as those at the recent United Nations Conference of the Parties (COP27).

The most recent Intergovernmental Panel on Climate Change (IPCC) report warned that policymakers have less than three years to act to avert catastrophic and irreversible changes to the world’s climate. The shared socioeconomic pathways (SSPs) they used to model future scenarios for climate change are based on factors like population, economic growth, education, urbanization and innovation. These new pathways illustrate a more complete picture of socioeconomic trends that could affect future greenhouse gas emissions.

Only recently have researchers been able to produce global predictions for total glacial mass change using the new SSPs. David Rounce, an assistant professor in CMU’s Department of Civil and Environmental Engineering, aggregated these future climate scenarios based on their increase in global mean temperature to evaluate the corresponding impacts associated with temperature change scenarios ranging from 1.5°C to 4°C. His model is also calibrated with an unprecedented amount of data, including individual mass-change observations for every glacier, and uses state-of-the-art calibration methods that require the use of supercomputers.

Rounce and his team found that in the SSPs with continued investment in fossil fuels, more than 40% of the glacial mass will be gone within the century, and more than 80% of glaciers by number could well disappear. Even in a best-case, low-emissions scenario, where the increase in global mean temperature is limited to 1.5°C relative to pre-industrial levels, more than 25% of glacial mass will be gone and nearly 50% of glaciers by number are projected to disappear. A majority of these lost glaciers are small (less than one square kilometer) by glacial standards, but their loss can negatively affect local hydrology, tourism, glacier hazards and cultural values.

Many processes govern how glaciers lose mass, and Rounce is working to advance how models account for different types of glaciers, including tidewater and debris-covered glaciers. Tidewater glaciers terminate in the ocean, which causes them to lose a lot of mass at this interface. Debris-covered glaciers are covered by sand, rocks and boulders. Prior work by Rounce has shown that the thickness and distribution of debris cover can have a positive or negative effect on glacial melt rates across an entire region, depending on the debris thickness. In this newest work, he found that accounting for these processes had relatively little impact on the global glacier projections but substantial differences in mass loss were found when analyzing individual glaciers.

Rounce’s work provides better context for regional glacier modeling, and he hopes it will spur climate policymakers to lower temperature-change goals beyond the 2.7°C mark that pledges from COP26 are projected to hit. Smaller glacial regions like Central Europe, low latitudes like the Andes, and the upper areas of North America will be disproportionately affected by temperatures rising more than 2°C. At a 3°C rise, these glacial regions almost completely disappear.

Rounce notes that glaciers take a long time to respond to climate change. He describes the glaciers as extremely slow-moving rivers. Cutting emissions today will not remove previously emitted greenhouse gases, nor can it instantly halt the inertia they contribute to climate change, meaning even a complete halt in emissions would still take between 30 and 100 years to be reflected in glacier mass loss rates.

To view the Global glacier change in the 21st century: Every increase in temperature matters study, click here.

Share this story:

About Author

mm
, editor-in-chief

Dan first joined UKi Media & Events in 2014 having spent the early years of his career in the recruitment industry. As editor, he now produces content for Meteorological Technology International, unearthing the latest technological advances and research methods for the publication of each exciting new issue. When he’s not reporting on the latest meteorological news, Dan can be found on the golf course or apprehensively planning his next DIY project.

Comments are closed.