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Glaciology / Climate history / Geology / Geochronology / Ice core / Incremental dating / Quelccaya Ice Cap / Isotope analysis / Byrd Polar Research Center / Historical geology / Physical geography / Water ice


tional processes must be quantified and taken into consideration when interpreting the results from the 205-meter and 202meter cores. The project was supported by National Science Foundation grant DPPThe Polar
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Document Date: 2011-05-06 15:42:21


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City

Hanover / Lincoln / /

Company

Bain / Quaternary Isotope Laboratory / /

Continent

Antarctica / /

Country

United States / Canada / United Kingdom / Peru / /

Facility

Siple Station / Amundsen-Scott South Pole Station / Scott Polar Research Institute / University of Calgary / Quaternary Isotope Laboratory / Astronomy University of Kansas Lawrence / University of Cambridge / MINZE STUIVER Quaternary Isotope Laboratory University of Washington Seattle / /

NaturalFeature

Vienna Standard Mean Ocean / /

Organization

Polar Ice Coring Office / National Science Foundation / University of Cambridge / Ohio State University / University of Calgary / MINZE STUIVER Quaternary Isotope Laboratory University of Washington Seattle / Washington / Polar Research Institute / Department of Physics / Physics and Astronomy University of Kansas Lawrence / Byrd Polar Research Center / Department of Polar Programs / /

Person

Drewry / PIETER M. GROOTES / Bruce Koci / El Nino / Erick Chiang / Travis Saling / Lee DeGalen / Jay Sonderup / Ron LaCount / David Bresnahan / CLAUDE M. LAIRD / John Litwak / EDWARD J. ZELLER / /

Position

Contractor / Major / Representative / D.J. / /

ProvinceOrState

Alberta / Kansas / Nebraska / New Hampshire / /

PublishedMedium

Journal of Geophysical Research / /

Region

Antarctic / East Antarctica / West Antarctica / /

Technology

sublimation / /

SocialTag