PP33A:
Reconstructing and Modeling Late Pliocene Climate Variability II Posters

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Session ID#: 13453

Session Description:
The Pliocene epoch (~2.6-5.3 million years ago) is arguably the best-resolved example of a climate state in long-term equilibrium with current or predicted near-future atmospheric CO2 concentrations. It was characterized by a warmer climate globally, reduced continental ice volume, and reduced ocean/atmosphere circulation intensity. Pleistocene paleoclimate studies have demonstrated the value of understanding climate variability on orbital timescales, whereby the unique spatial and temporal signatures of individual interglacials or glacial-interglacial cycles highlight sensitive regions or climate systems. Recent modeling work confirms that such variability (and regional non-synchronicity) should also be expected in the Pliocene.

As part of the PAGES PlioVAR working group, this session welcomes submissions which reconstruct and/or model mid and late Pliocene climates and environmental responses. Contributions investigating marine and terrestrial environmental change, ice-sheet behaviour, biotic responses and/or biogeochemical cycling are encouraged, so as to better understand climate forcings and feedbacks through both data analysis and data-model integration.

Primary Convener:  Erin McClymont, University of Durham, Durham, United Kingdom
Conveners:  Natalie Burls, George Mason University, Atmospheric, Oceanic and Earth Sciences, Fairfax, VA, United States and Heather L Ford, University of Cambridge, Earth Sciences, Cambridge, United Kingdom
Chairs:  Erin McClymont, University of Durham, Durham, United Kingdom, Heather L Ford, University of Cambridge, Earth Sciences, Cambridge, United Kingdom and Natalie Burls, George Mason University, Atmospheric, Oceanic and Earth Sciences, Fairfax, VA, United States
OSPA Liaison:  Heather L Ford, University of Cambridge, Earth Sciences, Cambridge, United Kingdom
Index Terms:

4912 Biogeochemical cycles, processes, and modeling [PALEOCEANOGRAPHY]
4928 Global climate models [PALEOCEANOGRAPHY]
4936 Interglacial [PALEOCEANOGRAPHY]
4950 Paleoecology [PALEOCEANOGRAPHY]

Abstracts Submitted to this Session:

Peter Jacobs1, Dr. Harry J Dowsett, PhD2 and Kim de Mutsert1, (1)George Mason University, Environmental Science and Policy, Fairfax, VA, United States, (2)USGS, Reston, VA, United States
Dr. Harry J Dowsett, PhD1, Aisling M Dolan2, David B Rowley3, Robert Moucha4, Alessandro M Forte5, Jerry X Mitrovica6, Matthew J Pound7, Ulrich Salzmann8, Marci M Robinson9, Mark A. Chandler10, Kevin Foley11, Alan Haywood2 and PRISM Project Team, (1)USGS, Eastern Geology and Paleoclimate Science Center, Reston, United States, (2)University of Leeds, Leeds, LS2, United Kingdom, (3)The University of Chicago, Department of the Geophysical Sciences, Chicago, IL, United States, (4)Syracuse University, Earth Sciences, Syracuse, NY, United States, (5)University of Quebec at Montreal UQAM, Montreal, QC, Canada, (6)Harvard University, Department of Earth and Planetary Sciences, Cambridge, United States, (7)Northumbria University, Department of Geography and Environmental Sciences, Newcastle-Upon-Tyne, United Kingdom, (8)Northumbria University, Department of Geography, Newcastle-Upon-Tyne, United Kingdom, (9)USGS, Florence Bascom Geoscience Center, Reston, United States, (10)CCSR / NASA GISS, Madison, WI, United States, (11)USGS, Eastern Geology and Paleoclimate Science Center, Reston, VA, United States
Deepak Chandan and W Richard Peltier, University of Toronto, Physics, Toronto, ON, Canada
Julia Claire Tindall, University of Leeds, Leeds, United Kingdom and Alan Haywood, University of Leeds, Leeds, LS2, United Kingdom
Ran Feng, National Center for Atmospheric Research, Boulder, CO, United States, Bette L Otto-Bliesner, NSF National Center for Atmospheric Research, Boulder, United States, Tamara Fletcher, Institute of Applied Ecology, Chinese Academy of Sciences, Missoula, MT, United States, Ashley Ballantyne, University of Montana, Missoula, MT, United States and Esther C Brady, National Center for Atmospheric Research, Climate and Global Dynamics Laboratory, Boulder, United States
Sarah M White, University of California Santa Cruz, Earth and Planetary Sciences, Santa Cruz, CA, United States and Ana Christina Ravelo, University of California-Santa Cruz, Santa Cruz, CA, United States
Montserrat Alonso-Garcia1,2, Emilia Salgueiro3,4, Teresa Rodrigues4,5, Carlos A Alvarez Zarikian6, Henning Kuhnert7, Ursula Roehl7, Antje H L Voelker5,8, Francisco J Sierro9 and Fatima F G Abrantes1,3, (1)Centro de Ciencias do Mar, Faro, Portugal, (2)Universidad de Salamanca, Geology Department, Salamanca, Spain, (3)Instituto Português do Mar e da Atmosfera, Lisboa, Portugal, (4)Centro de Ciencias do Mar (CCMAR), Faro, Portugal, (5)Instituto Português do Mar e da Atmosfera, Geologia e Georecursos Marinhos, Lisboa, Portugal, (6)Texas A&M University, College Station, TX, United States, (7)MARUM - University of Bremen, Bremen, Germany, (8)Centro de Ciencias do Mar (CCMAR/ CIMAR LA), Universidade do Algarve, Faro, Portugal, (9)University of Salamanca, Department of Geology, Salamanca, Spain
Resti Samyati Jatiningrum1, Tokiyuki Sato2 and Rendy Effendi2, (1)Akita University, Department of Geosciences, Geotechnology, and Material Resource Engineering, Akita, Japan, (2)Akita University, Faculty of International Resource Sciences, Akita, Japan