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UM Rosenstiel School Professor Joseph M. Prospero and colleagues Joanna E. Bullard and Richard Hodgkins (Loughborough University, U.K.) analyzed six years of dust concentrations collected at the Stórhöfoi research station on the island of Heimaey, which is located 17 km (10.5 mi) off the south coast of Iceland. The results show large increases in dust concentration, which can be traced to dust sources adjacent to major glaciers on Iceland.
As the glaciers melt, rivers of black, volcanic-rich sediments flow into the surrounding land and nearby ocean. Intense windstorms, common in the high-latitudes, eventually sweep up the dried sediments. The resulting dust storms are clearly visible in satellite images that show huge dust plumes extending hundreds of kilometers south over the Atlantic Ocean. Iceland glaciers are melting at a high rate due to global warming and to sub-glacial volcanic activity.
“The dust in Iceland dust storms can also have an impact on the glaciers themselves,” said Prospero, UM Rosenstiel professor emeritus and lead author on the study. “The black dust deposited on the glacier surface absorbs solar radiation thereby increasing the rates of glacial melting.”
Iceland dust can also affect ocean processes over the North Atlantic. The researchers suggest that the iron-rich dust provides a late summer/early fall nutrient boost to the typically iron-depleted North Atlantic Ocean waters. The iron increases the ocean’s primary productivity and stimulates the growth of marine biota. This, in turn, increases the draw down of CO2 from the atmosphere to the ocean....
The photographer, Ysangkok, says: Can't really remember what glacier it was, maybe it was Vatnajökull. Public domain
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