Late Quaternary glacial history constrains glacio-isostatic rebound in Enderby Land, East Antarctica

Duanne WHITE, David Fink

    Research output: Contribution to journalArticle

    3 Citations (Scopus)

    Abstract

    Measurements of the loss or gain of ice mass from large ice sheets are presently achieved through satellite-based techniques such as GRACE (Gravity Recovery and Climate Experiment). The accuracy of these satellite-based measurements to changes in modern ice sheet mass depends on our knowledge of present-day glacio-isostatic crustal uplift rates caused by past ice sheet changes. To improvemodels of glacio-isostatic rebound in East Antarctica, we investigated ice histories along Rayner Glacier, Enderby Land, and a little explored sector of the ice sheet where GRACE data had suggested significant mass gain during the last decade. Observations froma recent glacial geomorphic reconnaissance coupled with cosmogenic nuclide dating indicate that in the lower part of the Rayner Glacier, Enderby Land, ice heights lowered by at least 300m and the calving margin retreated by at least 10 km in the early Holocene (~6 to 9 ka B.P.). The magnitude and timing of deglaciation are consistent with ice histories used to model the postglacial rebound corrections for present-day GRACE mass trends. These observations strengthen the body of evidence that suggests ice mass gain in Enderby Land is presently partly offsetting mass loss in other parts of Antarctica.
    Original languageEnglish
    Pages (from-to)401-413
    Number of pages13
    JournalJournal of Geophysical Research: Earth Surface
    Volume119
    Issue number3
    DOIs
    Publication statusPublished - 2014

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    glacial history
    ice sheet
    GRACE
    ice
    glacier
    postglacial rebound
    history
    deglaciation
    Antarctica
    land
    uplift
    Holocene

    Cite this

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    title = "Late Quaternary glacial history constrains glacio-isostatic rebound in Enderby Land, East Antarctica",
    abstract = "Measurements of the loss or gain of ice mass from large ice sheets are presently achieved through satellite-based techniques such as GRACE (Gravity Recovery and Climate Experiment). The accuracy of these satellite-based measurements to changes in modern ice sheet mass depends on our knowledge of present-day glacio-isostatic crustal uplift rates caused by past ice sheet changes. To improvemodels of glacio-isostatic rebound in East Antarctica, we investigated ice histories along Rayner Glacier, Enderby Land, and a little explored sector of the ice sheet where GRACE data had suggested significant mass gain during the last decade. Observations froma recent glacial geomorphic reconnaissance coupled with cosmogenic nuclide dating indicate that in the lower part of the Rayner Glacier, Enderby Land, ice heights lowered by at least 300m and the calving margin retreated by at least 10 km in the early Holocene (~6 to 9 ka B.P.). The magnitude and timing of deglaciation are consistent with ice histories used to model the postglacial rebound corrections for present-day GRACE mass trends. These observations strengthen the body of evidence that suggests ice mass gain in Enderby Land is presently partly offsetting mass loss in other parts of Antarctica.",
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    author = "Duanne WHITE and David Fink",
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    Late Quaternary glacial history constrains glacio-isostatic rebound in Enderby Land, East Antarctica. / WHITE, Duanne; Fink, David.

    In: Journal of Geophysical Research: Earth Surface, Vol. 119, No. 3, 2014, p. 401-413.

    Research output: Contribution to journalArticle

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    AU - Fink, David

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