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Donald E. Voigt
Researcher at Pennsylvania State University
Publications - 30
Citations - 1833
Donald E. Voigt is an academic researcher from Pennsylvania State University. The author has contributed to research in topics: Ice core & Ice sheet. The author has an hindex of 18, co-authored 30 publications receiving 1626 citations.
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Journal ArticleDOI
Precise interpolar phasing of abrupt climate change during the last ice age
Christo Buizert,Betty Adrian,Jinho Ahn,Mary R. Albert,Richard B. Alley,Daniel Baggenstos,T. K. Bauska,R. C. Bay,Brian B. Bencivengo,Charles R. Bentley,Edward J. Brook,Nathan Chellman,Gary D. Clow,Jihong Cole-Dai,Howard Conway,Eric D. Cravens,Kurt M. Cuffey,Nelia W. Dunbar,J. S. Edwards,John M. Fegyveresi,D. G. Ferris,Joan J. Fitzpatrick,Tyler J. Fudge,Chris J. Gibson,Vasileios Gkinis,Vasileios Gkinis,Joshua J. Goetz,Stephanie Gregory,Geoffrey M. Hargreaves,Nels Iverson,Jay A. Johnson,Tyler R. Jones,M. Kalk,Matthew J. Kippenhan,B. G. Koffman,Karl J. Kreutz,Tanner W. Kuhl,Donald A. Lebar,James E. Lee,Shaun A. Marcott,Shaun A. Marcott,Bradley R. Markle,Olivia J. Maselli,Joseph R. McConnell,Kenneth C. McGwire,Logan Mitchell,Nicolai B. Mortensen,Peter Neff,Kunihiko Nishiizumi,Richard M. Nunn,Anais Orsi,Anais Orsi,Daniel R. Pasteris,Joel B Pedro,Joel B Pedro,Erin C. Pettit,P. Buford Price,John C. Priscu,Rachael H. Rhodes,Julia Rosen,Andrew J. Schauer,Spruce W. Schoenemann,Paul J. Sendelbach,Jeffrey P. Severinghaus,Alexander J. Shturmakov,Michael Sigl,Kristina Slawny,Joseph M. Souney,Todd Sowers,M. K. Spencer,Eric J. Steig,Kendrick C. Taylor,Mark S. Twickler,Bruce H. Vaughn,Donald E. Voigt,Edwin D. Waddington,Kees C. Welten,Anthony W. Wendricks,James W. C. White,Mai Winstrup,Mai Winstrup,G. J. Wong,Thomas E. Woodruff +82 more
TL;DR: A north-to-south directionality of the abrupt climatic signal is demonstrated, which is propagated to the Southern Hemisphere high latitudes by oceanic rather than atmospheric processes, which confirms a central role for ocean circulation in the bipolar seesaw.
Journal ArticleDOI
Onset of deglacial warming in West Antarctica driven by local orbital forcing
Tyler J. Fudge,Eric J. Steig,Bradley R. Markle,Spruce W. Schoenemann,Qinghua Ding,Kendrick C. Taylor,Joseph R. McConnell,Edward J. Brook,Todd Sowers,James W. C. White,Richard B. Alley,Hai Cheng,Hai Cheng,Gary D. Clow,Jihong Cole-Dai,Howard Conway,Kurt M. Cuffey,J. S. Edwards,R. Lawrence Edwards,Ross Edwards,John M. Fegyveresi,David G. Ferris,Joan J. Fitzpatrick,Jay A. Johnson,Geoffrey M. Hargreaves,James E. Lee,Olivia J. Maselli,William P. Mason,Kenneth C. McGwire,Logan Mitchell,Nicolai B. Mortensen,Peter Neff,Peter Neff,Anais Orsi,Trevor Popp,Andrew J. Schauer,Jeffrey P. Severinghaus,Michael Sigl,M. K. Spencer,Bruce H. Vaughn,Donald E. Voigt,Edwin D. Waddington,Xianfeng Wang,G. J. Wong +43 more
TL;DR: Results from a new, annually resolved ice-core record from West Antarctica suggest a more active role for the Southern Ocean in the onset of deglaciation than is inferred from ice cores in the East Antarctic interior, which are largely isolated from sea-ice changes.
Journal ArticleDOI
Chemical fixation of arsenic in contaminated soils
TL;DR: In this article, the chemistry of the fixation process used in the field is poorly understood and the intent of the first step is to form insoluble Fe arsenate, the second to bind the soil.
Journal ArticleDOI
Ice stream D flow speed is strongly modulated by the tide beneath the Ross Ice Shelf
TL;DR: In this paper, the flow velocity of ice stream D, West Antarctica has been measured to vary by a factor of three over the course of a day and these fluctuations are measured at the grounding line as well as upstream of the ground line in the ice plain of D. The diurnal velocity fluctuation appears to be driven by the tide beneath the Ross Ice Shelf.
Journal ArticleDOI
Continued deceleration of Whillans Ice Stream, West Antarctica
Ian Joughin,Robert Bindschadler,Matt A. King,Donald E. Voigt,Richard B. Alley,Sridhar Anandakrishnan,Huw J. Horgan,L. E. Peters,J. Paul Winberry,Sarah B. Das,Ginny A. Catania +10 more
TL;DR: In this paper, GPS data showed that the Whillans ice stream is continuing to decelerate at rates of about 0.6%/yr2, with faster rates near the grounding line.