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      <header>
        <identifier>doi:10.1594/pangaea.119750</identifier>
        <datestamp>2025-02-09T03:53:38Z</datestamp>
        <setSpec>PANGAEA</setSpec>
        <setSpec>PANGAEA.REPOSITORY</setSpec>
      </header>
      <metadata>
        <oai_dc:dc xmlns:dc="http://purl.org/dc/elements/1.1/" xmlns:oai_dc="http://www.openarchives.org/OAI/2.0/oai_dc/" xsi:schemaLocation="http://www.openarchives.org/OAI/2.0/oai_dc/ http://www.openarchives.org/OAI/2.0/oai_dc.xsd">
          <dc:title>Isotope values of fresh snow samples and daily temperature from Neumayer station in the period 1981-2000</dc:title>
          <dc:creator>Schlosser, Elisabeth</dc:creator>
          <dc:creator>Reijmer, Carleen H</dc:creator>
          <dc:creator>Oerter, Hans</dc:creator>
          <dc:creator>Graf, Wolfgang</dc:creator>
          <dc:publisher>PANGAEA</dc:publisher>
          <dc:date>2003</dc:date>
          <dc:date>Issued: 2003</dc:date>
          <dc:relation>doi:10.3189/172756404781814276</dc:relation>
          <dc:relation>doi:10.3189/002214308784408991</dc:relation>
          <dc:subject>DATE/TIME</dc:subject>
          <dc:subject>δ Deuterium</dc:subject>
          <dc:subject>δ18O, water</dc:subject>
          <dc:subject>Deuterium excess</dc:subject>
          <dc:subject>Temperature, air</dc:subject>
          <dc:subject>Research station</dc:subject>
          <dc:subject>Calculated</dc:subject>
          <dc:subject>Neumayer_based</dc:subject>
          <dc:subject>NEUMAYER III</dc:subject>
          <dc:subject>Glaciology @ AWI (AWI_Glac)</dc:subject>
          <dc:description>The relationship between d18O and air temperature at Neumayer station, Ekströmisen, Antarctica, was investigated using fresh-snow samples from the time period 1981-2000. A trajectory model that calculated 5 day-backward trajectories was used to study the influence of different synoptic weather situations and thus of different moisture sources on this correlation. Generally a high correlation between air temperature and d18O was found, but the quality of the d18O-T relationship varied with the different trajectory classes. Additionally, the sea-ice coverage on the travel path of the moist air was considered. The amount of open ocean water underneath the trajectory has a large influence on the d18O-T relationship. For trajectories that lead completely above open water, no significant correlation between d18O and T was found, because mixing with air masses containing additionally evaporated water vapour from the ocean influences the isotope ratio of precipitation. A very high correlation, however, was found for transports over the completely ice-covered Weddell Sea.</dc:description>
          <dc:description>Isotope measurements 1981-1999 by GSF, 2000 by AWI.</dc:description>
          <dc:description>Supplement to: Schlosser, Elisabeth; Reijmer, Carleen H; Oerter, Hans; Graf, Wolfgang (2004): The influence of origin of precipitation on the d18O-T relationship at Neumayer Station, Ekströmisen, Antarctica. Annals of Glaciology, 39, 41-48</dc:description>
          <dc:language>en</dc:language>
          <dc:type>Dataset</dc:type>
          <dc:type>Supplementary Dataset</dc:type>
          <dc:format>text/tab-separated-values</dc:format>
          <dc:rights>Creative Commons Attribution 3.0 Unported</dc:rights>
          <dc:rights>https://creativecommons.org/licenses/by/3.0/legalcode</dc:rights>
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