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      Johan Dahl Land, south Greenland: the end of a 20th century glacier expansion

      Polar Record
      Cambridge University Press (CUP)

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          Changes in the velocity structure of the Greenland Ice Sheet.

          Using satellite radar interferometry observations of Greenland, we detected widespread glacier acceleration below 66 degrees north between 1996 and 2000, which rapidly expanded to 70 degrees north in 2005. Accelerated ice discharge in the west and particularly in the east doubled the ice sheet mass deficit in the last decade from 90 to 220 cubic kilometers per year. As more glaciers accelerate farther north, the contribution of Greenland to sea-level rise will continue to increase.
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            Contrasting Response of South Greenland Glaciers to Recent Climatic Change

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              Holocene relative sea-level changes in the Qaqortoq area, southern Greenland

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                Author and article information

                Journal
                applab
                Polar Record
                Polar Record
                Cambridge University Press (CUP)
                0032-2474
                1475-3057
                October 2009
                September 4 2009
                October 2009
                : 45
                : 04
                : 337
                Article
                10.1017/S003224740900833X
                b2cccff8-321b-4242-b3ca-33646f246ff7
                © 2009
                History

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