Satellite measurements show that West Antarctica’s gravitational pull measurably decreased over three years because of lost mass due to melting ice, according to research published recently in the journal Geophysical Research Letters.
Data from the European Space Agency’s Gravity Field and Steady-State Ocean Circulation Explorer (GOCE), combined with “coarser” measurements from the NASA–German GRACE satellite, allowed scientists to look at changes in ice mass in small glacial systems and compare those to high-resolution measurements of Antarctica’s gravitational field.
“They have found that the loss of ice from West Antarctica between 2009 and 2012 caused a dip in the gravity field over the region,” according to a GOCE press release.
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