Andean glaciers advanced during an acute period of climate change at the end of the last Ice Age, new research led by Aberystwyth University has found.

An international team of glaciologists, led by Aberystwyth University, made the discovery as part of a new project into tropical glaciers in Peru.

The findings, published in ‘Nature Scientific Reports’, shed new light on how glaciers respond to shifting climate patterns and may help improve predictions of future climate impacts.

The study focused on the Younger Dryas period, a time of sudden and dramatic climate change that occurred approximately 12,900 to 11,700 years ago.

Contrary to previous theories, which suggest that glaciers in this area of Peru retreated during this time, the researchers found that those in the Santa Cruz Valley of Peru actually grew.

The glaciologists believe that this advance was driven by increased snowfall linked to seasonal shifts in the Intertropical Convergence Zone - a belt of low pressure that moves between the hemispheres and influences tropical weather patterns.

To reach their conclusions, the research team dated boulders transported and deposited by glaciers in the valley.

Once deposited, these boulders serve as physical evidence of glacial movement over millennia and provide insights into historical climate conditions.

Lead author Professor Neil Glasser from Aberystwyth University - a glacial geomorphologist who researches glacier change in southern South America - said: “Our study suggests that snowfall was a key factor driving glacier growth in the tropical Andes during the Younger Dryas.

“We were also able to date the timing of their advances more precisely than ever before.

“Our study shows that these glaciers are highly sensitive to climate shifts, particularly changes in precipitation patterns.

“Understanding the history of glacier advance and recession is really important because it helps us better anticipate how these glaciers will respond to future warming.”