E
E. D. Waddington
Researcher at University of Washington
Publications - 22
Citations - 2651
E. D. Waddington is an academic researcher from University of Washington. The author has contributed to research in topics: Ice core & Ice sheet. The author has an hindex of 17, co-authored 22 publications receiving 2574 citations.
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Journal ArticleDOI
Abrupt increase in Greenland snow accumulation at the end of the Younger Dryas event
Richard B. Alley,D. A. Meese,C. A. Shuman,Anthony J. Gow,Kendrick C. Taylor,Pieter Meiert Grootes,James W. C. White,M. Ram,E. D. Waddington,Paul Andrew Mayewski,Gregory A. Zielinski +10 more
TL;DR: In this article, the authors present results from a new Greenland ice core (GISP2) showing that snow accumulation doubled rapidly from the Younger Dryas event to the subsequent Preboreal interval, possibly in one to three years.
Journal ArticleDOI
The Accumulation Record from the GISP2 Core as an Indicator of Climate Change Throughout the Holocene.
D. A. Meese,Anthony J. Gow,Pieter Meiert Grootes,Minze Stuiver,Paul Andrew Mayewski,Gregory A. Zielinski,M. Ram,Kendrick C. Taylor,E. D. Waddington +8 more
TL;DR: A depth-age scale and an accumulation history for the Holocene have been established on the Greenland Ice Sheet Project 2 (GISP2) deep core, providing the most continuously dated record of annual layer accumulation currently available.
Journal ArticleDOI
Electrical conductivity measurements from the GISP2 and GRIP Greenland ice cores
Kendrick C. Taylor,Claus U. Hammer,Richard B. Alley,Henrik Clausen,Dorthe Dahl-Jensen,Anthony J. Gow,Niels S. Gundestrup,J. Kipfstuh,John C. Moore,John C. Moore,E. D. Waddington +10 more
TL;DR: In this article, electrical conductivity records for the Greenland Ice Sheet Project 2 (GISP2) and Greenland Ice-core Project (GRIP) ice cores, drilled 28 km apart to enable direct comparison of the results.
Journal ArticleDOI
Distortion of isochronous layers in ice revealed by ground-penetrating radar
TL;DR: In this article, ground-penetrating radar data from Fletcher Promontory, Antarctica is used to detect arches and troughs in isochronous ice layers to a depth of 100m.
Journal ArticleDOI
Possible displacement of the climate signal in ancient ice by premelting and anomalous diffusion.
TL;DR: It is shown that premelting influences compositional diffusion in a manner that causes the advection of impurity anomalies towards warmer regions while maintaining their spatial integrity.