Cosmogenic nuclides constrain surface fluctuations of an East Antarctic outlet glacier since the Pliocene.

Article OPEN
R. S. Jones; K. P. Norton; A. N. Mackintosh; J. T. H. Anderson; P. Kubik; C. Vockenhuber; H. Wittmann; D. Fink; G. S. Wilson; N. R. Golledge; R. McKay;

Understanding past changes in the Antarctic ice sheets provides insight into how they might respond to future climate warming. During the Pliocene and Pleistocene, geological data show that the East Antarctic Ice Sheet responded to glacial and interglacial cycles by rem... View more
Share - Bookmark