Slush holds 2x more meltwater, risks Antarctic ice shelf stability, AI reveals

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Antarctica,Climate Change,Energy &Amp

Slush comprises twice as much meltwater as previously known, which is influencing ice shelf stability and contributing to sea level rise.

Pooled meltwater and slush on the Tracy Tremenchus Ice Shelf, which flows into the Southern Ocean. Contains modified Copernicus Sentinel data .Artificial intelligence has been used to aid in various scientific developments recently. Now scientists have employed AI to investigate the role of slush—water-soaked snow—on Antarctic ice shelves during the summer months.

“When traditional meltwater mapping methods are used it can be confused for cloud shadow, snow, and ponded water. This means we haven’t been able to map it on a large scale, and if we can’t map it, it is very difficult to understand and track!” “This accuracy reflects the subjective nature of mapping slush itself, it is very hard to distinguish when slush becomes ponded water and vice versa.”

“When an ice shelf melts, if there is pore space in the snow or firn, the meltwater will fill these spaces first. Once the snow/firn is fully saturated, any further meltwater has nowhere to go, and it will likely pond or form surface streams and rivers on the ice shelf.”

 

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