Ryan Glaubke received his Ph.D. from Rutgers University before joining the Paleo2 Lab in the Fall of 2024. He is broadly interested in the reconstructing past ocean conditions from periods of Earth’s history that could serve as “natural analogues” to the rate and magnitude of modern climate change. At Rutgers, Ryan’s dissertation work focused on the role ocean circulation played in the rise of atmospheric CO₂ concentrations across the last major example of global warming—the Last Deglaciation. At Old Dominion University, where Ryan received his B.S. and M.S. degrees, he investigated the response of the El Niño system—the world’s largest and most globally significant recurring climate pattern—to episodes of meltwater discharge across abrupt climate events in the deglacial period. Now, at the University of Arizona, Ryan is investigating whether the Indian Ocean supported a new and potentially significant mode of climate variability during the Pliocene—a warm period approximately 3 million years ago that resembles Earth’s future climate. Together, Ryan hopes these lessons from the past will help inform our projections of future change.
Personal interests: Hiking, surfing, soccer, music, and reading.
Email: glaubke@arizona.edu
Online presence: Bluesky, ResearchGate, Google Scholar