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Scientists Anthony Long and Sarah Woodroffe of Durham University geography department looking at glacial marine sediments near Ilulissat on Greenland. For the last 4 years they have been studying isostatic rebound or how the land is rising after the weight of ice is taken off it. If they can understand how the relative sea levels were affected by the changeing climate of the past they should be able to greater understand how the melting of the Greenland ice sheet will affect global sea levels. This understanding is crucial as the Greenland ice sheet contains enough warter to raise global sea levels by nine metres.
Science
scientist
study
research
Ilulissat
Greenland
glaciology
glaciologist
ice age
ice sheet
sediments
glacial marine sediment
sediment
deposits
isostatic rebound
sea level
sea level rise
long term study
understanding
interpret
interpretation
geography
university
geomorphology
Durham university
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