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Growing concerns about the timing, scale, and pace of future climate shifts underscore the need for a thorough grasp of the mechanisms driving climate variability. The discovery of significant abrupt climate changes in paleoclimate records—more extreme than those witnessed in modern times—has emphasized the dangers posed by rising greenhouse gas concentrations. Researchers employ diverse methods, from contemporary observations and process studies to paleoclimate proxies and model-based data analysis, to pinpoint triggers of sudden climate shifts. These insights enhance our capacity to forecast future trends. Current models still fall short in fully explaining climate variability across all timescales, partly because key relationships between climate and environmental feedbacks remain unclear. Developing hypotheses that connect climate forcings to their effects is especially vital for the Southern Hemisphere, where high-resolution paleoclimate data and detailed glaciological studies are scarce. Furthermore, studying how past societies adapted to climate shifts helps us anticipate the societal consequences of environmental challenges like shifting weather patterns and sea-level rise. Geoarchaeology, as an interdisciplinary field, allows us to explore these events through a human lens, offering insights into how future changes might influence cultural adaptation. The School of Earth and Climate Sciences and Climate Change Institute are renowned pioneers in these domains, having shaped key theories on global and abrupt climate change. In the coming years, faculty from both institutions will play central—and often leading—roles in climate research projects spanning deep ice core extraction, geological surveys, satellite remote sensing, and investigations into human-climate interactions.