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  • Antarctica; Area/locality; Beryllium-10; Beryllium-10, standard deviation; Correction; ELEVATION; Exposure age; Exposure age, standard deviation; ICEM; Ice measurement; LATITUDE; LONGITUDE; Reedy_Glacier; Sample comment; Sample ID  (2)
  • Amundsen Sea  (1)
  • Antarctica; ICEM; Ice measurement; International Polar Year (2007-2008); ipy; IPY; Reedy_Glacier  (1)
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  • 1
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    PANGAEA
    In:  Supplement to: Todd, Claire E; Stone, John O; Conway, Howard; Hall, Brenda L; Bromley, Gordon RM (2010): Late Quaternary evolution of Reedy Glacier, Antarctica. Quaternary Science Reviews, 29(11-12), 1328-1341, https://doi.org/10.1016/j.quascirev.2010.02.001
    Publikationsdatum: 2024-03-09
    Beschreibung: Fresh deposits above the margins of Reedy Glacier show that maximum ice levels during the last glaciation were several hundred meters above present near the glacier mouth and converged to less than 60 m above the present-day surface at the head of the glacier. Exposure ages of samples from five sites along its margin show that Reedy Glacier and its tributaries thickened asynchronously between 17 and 7 kyr BP At the Quartz Hills, located midway along the glacier, maximum ice levels were reached during the period 17-14 kyr BP. Farther up-glacier the ice surface reached its maximum elevation more recently: 14.7-10.2 kyr BP at the Caloplaca Hills; 9.1-7.7 kyr BP at Mims Spur; and around 7 kyr BP at Hatcher Bluffs. We attribute this time-transgressive behavior to two different processes: At the glacier mouth, growth of grounded ice and subsequent deglaciation in the Ross Sea embayment caused a wave of thickening and then thinning to propagate up-glacier. During the Lateglacial and Holocene, increased snow accumulation on the East Antarctic Ice Sheet caused transient thickening at the head of the glacier. An important result of this work is that moraines deposited along Reedy Glacier during the last ice age cannot be correlated to reconstruct a single glacial maximum longitudinal profile. The profile steepened during deglaciation of the Ross Sea, thinning at the Quartz Hills after 13 kyr BP while thickening upstream. Near its confluence with Mercer Ice Stream, rapid thinning beginning prior to 7-8 kyr BP reduced the level of Reedy Glacier to close to its present level. Thinning over the past 1000 years has lowered the glacier by less than 20 m.
    Schlagwort(e): Antarctica; ICEM; Ice measurement; International Polar Year (2007-2008); ipy; IPY; Reedy_Glacier
    Materialart: Dataset
    Format: application/zip, 2 datasets
    Standort Signatur Erwartet Verfügbarkeit
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  • 2
    Publikationsdatum: 2024-03-09
    Schlagwort(e): Antarctica; Area/locality; Beryllium-10; Beryllium-10, standard deviation; Correction; ELEVATION; Exposure age; Exposure age, standard deviation; ICEM; Ice measurement; LATITUDE; LONGITUDE; Reedy_Glacier; Sample comment; Sample ID
    Materialart: Dataset
    Format: text/tab-separated-values, 324 data points
    Standort Signatur Erwartet Verfügbarkeit
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  • 3
    Publikationsdatum: 2024-03-09
    Schlagwort(e): Antarctica; Area/locality; Beryllium-10; Beryllium-10, standard deviation; Correction; ELEVATION; Exposure age; Exposure age, standard deviation; ICEM; Ice measurement; LATITUDE; LONGITUDE; Reedy_Glacier; Sample comment; Sample ID
    Materialart: Dataset
    Format: text/tab-separated-values, 444 data points
    Standort Signatur Erwartet Verfügbarkeit
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  • 4
    Publikationsdatum: 2022-05-25
    Beschreibung: Author Posting. © American Geophysical Union, 2013. This article is posted here by permission of American Geophysical Union for personal use, not for redistribution. The definitive version was published in Journal of Geophysical Research 118 (2013): 118–130, doi:10.1029/2012JC008077.
    Beschreibung: Our understanding of past sea-ice variability is limited by the short length of satellite and instrumental records. Proxy records can extend these observations but require further development and validation. We compare methanesulfonic acid (MSA) and chloride (Cl–) concentrations from a new firn core from coastal West Antarctica with satellite-derived observations of regional sea-ice concentration (SIC) in the Amundsen Sea (AS) to evaluate spatial and temporal correlations from 2002–2010. The high accumulation rate (~39 g∙cm–2∙yr–1) provides monthly resolved records of MSA and Cl–, allowing detailed investigation of how regional SIC is recorded in the ice-sheet stratigraphy. Over the period 2002–2010 we find that the ice-sheet chemistry is significantly correlated with SIC variability within the AS and Pine Island Bay polynyas. Based on this result, we evaluate the use of ice-core chemistry as a proxy for interannual polynya variability in this region, one of the largest and most persistent polynya areas in Antarctica. MSA concentrations correlate strongly with summer SIC within the polynya regions, consistent with MSA at this site being derived from marine biological productivity during the spring and summer. Cl– concentrations correlate strongly with winter SIC within the polynyas as well as some regions outside the polynyas, consistent with Cl– at this site originating primarily from winter sea-ice formation. Spatial correlations were generally insignificant outside of the polynya areas, with some notable exceptions. Ice-core glaciochemical records from this dynamic region thus may provide a proxy for reconstructing AS and Pine Island Bay polynya variability prior to the satellite era.
    Beschreibung: This research was supported by an award from the Department of Energy Office of Science Graduate Fellowship Program (DOE SCGF) to ASC, a James E. and Barbara V. Moltz Research Fellowship to SBD, and by grants from NSF-OPP (#ANT-0632031 & #ANT-0631973); NSF-MRI (#EAR-1126217); NASA Cryosphere Program (#NNX10AP09G); and a WHOI Andrew W. Mellon Foundation Award for Innovative Research.
    Beschreibung: 2013-07-25
    Schlagwort(e): Sea ice ; Polynyas ; Antarctica ; Amundsen Sea ; Pine Island Bay ; Methanesulfonic acid
    Repository-Name: Woods Hole Open Access Server
    Materialart: Article
    Format: application/pdf
    Standort Signatur Erwartet Verfügbarkeit
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