PP037
The stability, structure and temporal variability of AMOC: past, present, and future
The stability, structure and temporal variability of AMOC: past, present, and future
Session ID#: 75841
Session Description:
The Atlantic Meridional Overturning Circulation (AMOC) is recognized as a major regulator for the Earth’s climate. Paleoclimate reconstructions applying diverse proxies have highlighted the close link between past climate change and ocean circulation dynamics, particularly in the Atlantic Ocean. Recent advancements in model simulations and contemporary observations have greatly grown our understanding and appreciation of the spatially and highly complex structure and temporal variability of the AMOC, and its interplay with the cryosphere. Yet, our ability to predict future AMOC response to anthropogenic forcing remains limited. An improved understanding of the AMOC’s response to hydrographic and climatic changes is hence critical. This session welcomes both modeling studies and proxy-reconstructions that investigate the relevance of AMOC changes for past climate change throughout the Quaternary, including drivers, and associated climate feedbacks over decadal-to-orbital timescales. Contributions that connect past AMOC evolution to the projected changes under future warmer climate are also welcomed.
Index Terms:
4532 General circulation [OCEANOGRAPHY: PHYSICAL]
4901 Abrupt/rapid climate change [PALEOCEANOGRAPHY]
4928 Global climate models [PALEOCEANOGRAPHY]
4962 Thermohaline [PALEOCEANOGRAPHY]
Primary Convener: Jerry Tjiputra, NORCE Norwegian Research Centre and Bjerknes Centre for Climate Research, Bergen, Norway
Conveners: Feng He, University of Wisconsin Madison, Madison, WI, United States, Julia Gottschalk, Lamont -Doherty Earth Observatory, Palisades, United States and Jerry F McManus, Columbia U. / LDEO, Palisades, NY, United States
Primary Liaison: Feng He, University of Wisconsin Madison, Madison, WI, United States
See more of: Paleoceanography and Paleoclimatology
