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    Multi-decadal record of ice dynamics on Daugaard Jensen Gletscher, East Greenland, from satellite imagery and terrestrial measurements

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    StearnsL_AoG_42(1)53.pdf (404.2Kb)
    Issue Date
    2005-08-01
    Author
    Stearns, Leigh A.
    Hamilton, Gordon S.
    Reeh, Niels
    Publisher
    International Glaciological Society
    Type
    Article
    Article Version
    Scholarly/refereed, publisher version
    Metadata
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    Abstract
    The history of ice velocity and calving front position of Daugaard Jensen Gletscher, a large outlet glacier in East Greenland, is reconstructed from field measurements, aerial photography and satellite imagery for the period 1950–2001. The calving terminus of the glacier has remained in approximately the same position over the past ∼50 years. There is no evidence of a change in ice motion between 1968 and 2001, based on a comparison of velocities derived from terrestrial surveying and feature tracking using sequential satellite images. Estimates of flux near the entrance to the fjord vs snow accumulation in the interior catchment show that Daugaard Jensen Gletscher has a small negative mass balance. This result is consistent with other mass-balance estimates for the inland region of the glacier.
    Description
    This is the publisher's version, also available electronically from "http://www.ingentaconnect.com".
    URI
    http://hdl.handle.net/1808/17211
    DOI
    https://doi.org/10.3189/172756405781812565
    ISSN
    0260-3055
    Collections
    • Geology Scholarly Works [245]
    Citation
    Stearns, L., Hamilton, G., & Reeh, N. (2005). Multi-decadal record of ice dynamics on Daugaard Jensen Gletscher, East Greenland, from satellite imagery and terrestrial measurements. Annals of Glaciology, 42(1), 53-58. http://dx.doi.org/10.3189/172756405781812565

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    Contact KU ScholarWorks
    785-864-8983
    KU Libraries
    1425 Jayhawk Blvd
    Lawrence, KS 66045
    785-864-8983

    KU Libraries
    1425 Jayhawk Blvd
    Lawrence, KS 66045
    Image Credits
     

     

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