The effect of Late Holocene ice-mass changes on glacial isostatic adjustment in West Antarctica
Glacial isostatic adjustment (GIA) describes the Earth’s response to changing ice and water loads as ice sheets grow and diminish. GIA is difficult to model in Antarctica due to limited knowledge of ice history and Earth properties. The signal confounds satellite gravity measurements of present-day...
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University of Newcastle upon Tyne
2014
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| Online Access: | http://ethos.bl.uk/OrderDetails.do?uin=uk.bl.ethos.664655 |