D-O Variability in Greenland Summit δ<sup>18</sup>O<sub>p</sub> Controlled by Southern Extent of Sea Ice in the North Atlantic During the Last Glacial.

Niezgoda, Kyle

D-O Variability in Greenland Summit δ¹⁸O_p Controlled by Southern Extent of Sea Ice in the North Atlantic During the Last Glacial.

Kyle Niezgoda¹, Christo Buizert², Kaden Martin² and David Noone³, (1)Oregon State University, College of Earth, Ocean, and Atmospheric Science, Corvallis, OR, United States, (2)Oregon State University, College of Earth, Ocean, and Atmospheric Sciences, Corvallis, OR, United States, (3)University of Auckland, Department of Physics, Auckland, New Zealand

D-O Variability in Greenland Summit δ18Op Controlled by Southern Extent of Sea Ice in the North Atlantic During the Last Glacial.

D-O Variability in Greenland Summit δ¹⁸O_p Controlled by Southern Extent of Sea Ice in the North Atlantic During the Last Glacial.