Asynchronous response to late Holocene cooling by glaciers in the Atlantic and Pacific sectors of the Arctic explained by weakening AMOC and intensified Aleutian Low: a data-model comparison


Gifford H Miller, University of Colorado, INSTAAR and Geological Sciences, Boulder, United States, Yafang Zhong, University of Wisconsin-Madison, CIMSS/SSEC, Madison, United States, Alexandra Jahn, University of Colorado Boulder, Atmospheric and Oceanic Sciences and Institute of Arctic and Alpine Research (INSTAAR), Boulder, United States, Aslaug Geirsdottir, University of Iceland, Department of Earth Sciences, Reykjavik, Iceland, Jason P Briner, University at Buffalo, Department of Earth Sciences, Buffalo, United States and Avriel D Licciardi, Accdon, Waltham, MA, United States
Back to: Temporal and Geographical Phasing of Northern Hemisphere Climate Change I