Water stable isotope record of ice core WAIS divide

Changes in atmospheric circulation over the past five decades have enhanced the wind-driven inflow of warm ocean water onto the Antarctic continental shelf, where it melts ice shelves from below. Atmospheric circulation changes have also caused rapid warming over the West Antarctic Ice Sheet, and co...

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Bibliographic Details
Main Authors: Steig, Eric J, Ding, Quinghua, White, James W C, Küttel, Meinrad, Rupper, Summer B, Neumann, T A, Neff, Peter D, Gallant, Ailie J E, Mayewski, Paul Andrew, Taylor, Kendrick C, Hoffmann, Georg, Dixon, Daniel A, Schoenemann, Spruce W, Markle, Bradley R, Fudge, Tyler J, Schneider, David P, Schauer, Andrew J, Teel, Rebecca P, Vaughn, Bruce H, Burgener, Landon, Williams, Jessica, Korotkikh, Elena, Gkinis, Vasileios
Format: Dataset
Language:English
Published: PANGAEA 2018
Subjects:
Online Access:https://doi.pangaea.de/10.1594/PANGAEA.886046
https://doi.org/10.1594/PANGAEA.886046