Wednesday, November 21, 2018

Glaciers Created a Huge 'Flour' Dust Storm in Greenland






















Researchers have written and speculated about glacier-flour dust storms in Greenland for a long time, according to NASA. But it took until this September for investigators to spot such a massive plume of the elusive dust forming and drifting 80 miles (130 kilometers) northwest of the far-northern village of Ittoqqortoormiit. Glacier flour is a fine dust created when glaciers pulverize rocks, NASA wrote. While satellites had occasionally spotted smaller storms of the stuff, this one was "by far the largest." 



The flour storm formed when a summer floodplain in the region dried out with late September's colder weather, leaving behind a large deposit of sediment carried south from more-northern glaciers.


According to NASA, storms like this are interesting because researchers just don't know much about them or how they affect the climate. While large dust storms found closer to the equator have known climate impacts, the role of glacial flour remains a mystery.

















































































































































































































































































































































































































































































































































































































































































































































































































































































































































































































































































































































































































































































































































































































































































































































































































































































































































































































































































































































































































































































































































































































































































































































































































































































































































































































































































































































































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