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  <dc:title xmlns:dc="http://purl.org/dc/elements/1.1/" xmlns:ows="http://www.opengis.net/ows">TALDICE, Antarctica 2,000 Year Ice Core Oxygen Isotope Data</dc:title>
  <dc:creator xmlns:dc="http://purl.org/dc/elements/1.1/" xmlns:ows="http://www.opengis.net/ows">Stenni, B.</dc:creator>
  <dc:creator xmlns:dc="http://purl.org/dc/elements/1.1/" xmlns:ows="http://www.opengis.net/ows">Stenni, B.</dc:creator>
  <dc:subject xmlns:dc="http://purl.org/dc/elements/1.1/" xmlns:ows="http://www.opengis.net/ows">earth science/paleoclimate/ice cores (age,null,null,year Common Era,null,ice cores,null,null,N,null)</dc:subject>
  <dc:subject xmlns:dc="http://purl.org/dc/elements/1.1/" xmlns:ows="http://www.opengis.net/ows">earth science/paleoclimate/ice cores (delta 18O,bulk ice,null,per mil SMOW,null,ice cores,null,isotope ratio mass spectrometry,N,uncertainty 0.05 per mil (+/-))</dc:subject>
  <dc:subject xmlns:dc="http://purl.org/dc/elements/1.1/" xmlns:ows="http://www.opengis.net/ows">earth science/paleoclimate/ice core</dc:subject>
  <dc:subject xmlns:dc="http://purl.org/dc/elements/1.1/" xmlns:ows="http://www.opengis.net/ows"> (Talos Dome TALDICE&gt;LATITUDE -72.8166&gt;LONGITUDE 159.1833)</dc:subject>
  <dc:description xmlns:dc="http://purl.org/dc/elements/1.1/" xmlns:ows="http://www.opengis.net/ows">Ice-core records of climate from Greenland and Antarctica show 
asynchronous temperature variations on millennial timescales 
during the last glacial period. The warming during the transition 
from glacial to interglacial conditions was markedly different 
between the hemispheres, a pattern attributed to the thermal 
bipolar see-saw. However, a record from the Ross Sea sector 
of East Antarctica has been suggested to be synchronous with 
Northern Hemisphere climate change.  Here we present a temperature 
record from the Talos Dome ice core, also located in the Ross Sea 
sector. We compare our record with ice-core analyses from Greenland, 
based on methane synchronization, and find clearly asynchronous 
temperature changes during the deglaciation. We also find distinct 
differences in Antarctic records, pointing to differences in the 
climate evolution of the Indo-Pacific and Atlantic sectors of 
Antarctica. In the Atlantic sector, we find that the rate of 
warming slowed between 16,000 and 14,500 years ago, parallel 
with the deceleration of the rise in atmospheric carbon dioxide 
concentrations and with a slight cooling over Greenland. 
In addition, our chronology supports the hypothesis that the 
cooling of the Antarctic Cold Reversal is synchronous with the 
Bølling-Allerød warming in the northern hemisphere 14,700 years ago. 
          STUDY NOTES: Ice Core oxygen isotope (d18O) data from the TALDICE ice core, Antarctica, for the paast 2,000 years.  </dc:description>
  <dc:publisher xmlns:dc="http://purl.org/dc/elements/1.1/" xmlns:ows="http://www.opengis.net/ows">NCDC-Paleoclimatology</dc:publisher>
  <dc:publisher xmlns:dc="http://purl.org/dc/elements/1.1/" xmlns:ows="http://www.opengis.net/ows">https://www.ncdc.noaa.gov/data-access/paleoclimatology-data - Bauer Bruce</dc:publisher>
  <dc:contributor xmlns:dc="http://purl.org/dc/elements/1.1/" xmlns:ows="http://www.opengis.net/ows">Investigator : Stenni, B.</dc:contributor>
  <dc:date xmlns:dc="http://purl.org/dc/elements/1.1/" xmlns:ows="http://www.opengis.net/ows">2017-05-19</dc:date>
  <dc:type xmlns:dc="http://purl.org/dc/elements/1.1/" xmlns:ows="http://www.opengis.net/ows">ONLINE Files</dc:type>
  <dc:format xmlns:dc="http://purl.org/dc/elements/1.1/" xmlns:ows="http://www.opengis.net/ows">online, ASCII</dc:format>
  <dc:identifier xmlns:dc="http://purl.org/dc/elements/1.1/" xmlns:ows="http://www.opengis.net/ows">https://www.ncdc.noaa.gov/paleo/study/22502</dc:identifier>
  <dc:identifier xmlns:dc="http://purl.org/dc/elements/1.1/" xmlns:ows="http://www.opengis.net/ows">https://www1.ncdc.noaa.gov/pub/data/paleo/icecore/antarctica/talos/taldice2010d18o2k.txt</dc:identifier>
  <dc:source xmlns:dc="http://purl.org/dc/elements/1.1/" xmlns:ows="http://www.opengis.net/ows">https://www1.ncdc.noaa.gov/pub/data/paleo/icecore/antarctica/talos/taldice2010d18o2k.txt</dc:source>
  <dc:language xmlns:dc="http://purl.org/dc/elements/1.1/" xmlns:ows="http://www.opengis.net/ows">English</dc:language>
  <dc:relation xmlns:dc="http://purl.org/dc/elements/1.1/" xmlns:ows="http://www.opengis.net/ows">https://www.ncdc.noaa.gov/paleo/study/22502</dc:relation>
  <dc:relation xmlns:dc="http://purl.org/dc/elements/1.1/" xmlns:ows="http://www.opengis.net/ows">https://www1.ncdc.noaa.gov/pub/data/paleo/icecore/antarctica/talos/taldice2010d18o2k.txt</dc:relation>
  <dc:relation xmlns:dc="http://purl.org/dc/elements/1.1/" xmlns:ows="http://www.opengis.net/ows">Stenni, B., D. Buiron, M. Frezzotti, S. Albani, C. Barbante, E. Bard, 
J.M. Barnola, M. Baroni, M. Baumgartner, M. Bonazza, E. Capron, 
E. Castellano, J. Chappellaz, B. Delmonte, S. Falourd, L. Genoni, 
P. Iacumin, J. Jouzel, S. Kipfstuhl, A. Landais, B. Lemieux-Dudon, 
V. Maggi, V. Masson-Delmotte, C. Mazzola, B. Minster, M. Montagnat, 
R. Mulvaney, B. Narcisi, H. Oerter, F. Parrenin, J.R. Petit, C. Ritz, 
C. Scarchilli, A. Schilt, S. Schüpbach, J. Schwander, E. Selmo, 
M. Severi, T.F. Stocker, and R. Udisti. 2010. 
Expression of the bipolar see-saw in Antarctic climate records 
during the last deglaciation. 
Nature Geoscience, Published online 5 December 2010. 
DOI: 10.1038/NGEO1026</dc:relation>
  <dc:coverage xmlns:dc="http://purl.org/dc/elements/1.1/" xmlns:ows="http://www.opengis.net/ows">START YEAR: 4 AD  * END YEAR: 1990 AD</dc:coverage>
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