Glaciers’ Cooling Effect May Delay Warming—But Not for Long
New research reveals that glaciers possess a surprising ability to temporarily cool the air around them, creating a localized buffer against global warming. This self-cooling mechanism, driven by katabatic winds, has been observed to reach its peak and is expected to change dramatically over the next two decades. As glaciers continue to lose mass, scientists warn that their capacity for cooling will diminish—leading to faster warming and accelerated melting. The Hidden Mechanism Behind Glacier Self-Cooling Glaciers are not just frozen reservoirs of water—they are dynamic systems that interact continuously with the atmosphere. According to a recent study by researchers from the University of Alaska Fairbanks and National Geographic researchers, katabatic winds—dense, cold air descending from glacier surfaces—help stabilize local temperatures by displacing warmer air masses. This natural process can slow regional warming, buying time before irreversible melti...