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Duo Chan
University of SouthamptonMeeting roles in:
Steadier and Faster Global Warming Since 1850 from Integrating Instrumental Data, Proxies, and Simple Theory
Assessing the Sensitivity of Paleoclimate Data Assimilation on the Great Barrier Reef Using Synthetic Coral Proxy Records of Sea Surface Temperature
Subpolar North Atlantic cooling reinforced by colder, drier atmosphere with a weakening AMOC
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