More from the article...
... In the summer of 2022, I skied across the flat, smooth, and white plateau of the icefield, accompanied by other researchers, sliding in the tracks of the person in front of me under a hot sun. From that plateau, around 40 huge, interconnected glaciers descend towards the sea, with hundreds of smaller glaciers on the mountain peaks all around.
Our work, now published in Nature Communications, has shown that Juneau is an example of a climate "feedback" in action: as temperatures are rising, less and less snow is remaining through the summer (technically: the "end-of-summer snowline" is rising). This in turn leads to ice being exposed to sunshine and higher temperatures, which means more melt, less snow, and so on.
Like many Alaskan glaciers, Juneau's are top-heavy, with lots of ice and snow at high altitudes above the end-of-summer snowline. This previously sustained the glacier tongues lower down. But when the end-of-summer snowline does creep up to the top plateau, then suddenly a large amount of a top-heavy glacier will be newly exposed to melting.
That's what's happening now, each summer, and the glaciers are melting much faster than before, causing the icefield to get thinner and thinner and the plateau to get lower and lower. Once a threshold is passed, these feedbacks can accelerate melt and drive a self-perpetuating loss of snow and ice which would continue even if the world were to stop warming.
Ice is melting faster than ever ...
