Quantifying Tidewater Glacier-Fjord Environments in the Rapidly Changing Regions of West and South Greenland
The Greenland Ice Sheet has undergone rapid mass loss over the last four decades, primarily through solid and liquid discharge at marine-terminating outlet glaciers. The acceleration of these glaciers is in part due to the increase in temperature of ocean water in contact with the glacier terminus....
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DigitalCommons@UMaine
2023
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Online Access: | https://digitalcommons.library.umaine.edu/etd/3921 https://digitalcommons.library.umaine.edu/context/etd/article/4965/viewcontent/M_Baratta_Sydney_Dec23.pdf |