Phys.org  October 22, 2024 Reconstructions of Earth’s past climate show evidence for instability and abrupt change, which are of great scientific and societal importance. The Dansgaard–Oeschger (DO) oscillation of the last Ice Age, which is most clearly observed in Greenland ice cores, is the prime example of such instability. An international team of researchers (Oregon State University, Pennsylvania State University, University of Miami, University of Colorado, Denmark, UK) presented ice-core records from south and coastal east Greenland to calibrate the local water isotope thermometer and provided a Greenland-wide spatial characterization of DO event magnitude. They used a series of idealized […]