The PRISM4 (mid-Piacenzian) paleoenvironmental reconstruction
Harry Dowsett1,Aisling Dolan2,David Rowley3,Robert Moucha4,Alessandro M. Forte5,6,Jerry X. Mitrovica7,Matthew Pound8,Ulrich Salzmann8,Marci Robinson1,Mark Chandler9,10,Kevin Foley1,and Alan Haywood2Harry Dowsett et al. Harry Dowsett1,Aisling Dolan2,David Rowley3,Robert Moucha4,Alessandro M. Forte5,6,Jerry X. Mitrovica7,Matthew Pound8,Ulrich Salzmann8,Marci Robinson1,Mark Chandler9,10,Kevin Foley1,and Alan Haywood2
1Eastern Geology and Paleoclimate Science Center, United States
Geological Survey, Reston, VA 20192, USA
2School of Earth and Environment, University of Leeds, Leeds LS2
9JT,
UK
3Department of the Geophysical Sciences, University of Chicago,
Chicago, IL 60637, USA
4Department of Earth Sciences, Syracuse University, Syracuse,
NY 13244,
USA
5Department of Geological Sciences, University of Florida, Gainesville,
FL 32611, USA
6GEOTOP, Université du Québec à Montréal, Montréal
QC, H3C 3P8, Canada
7Department of Earth and Planetary Sciences, Harvard University,
Cambridge, MA 02138, USA
8Department of Geography, Faculty of Engineering and Environment,
Northumbria University, Newcastle upon Tyne NE1 8ST, UK
9Center for Climate Systems Research at Columbia University, New York,
NY, USA
10NASA Goddard Institute for Space Studies, New York, NY, USA
1Eastern Geology and Paleoclimate Science Center, United States
Geological Survey, Reston, VA 20192, USA
2School of Earth and Environment, University of Leeds, Leeds LS2
9JT,
UK
3Department of the Geophysical Sciences, University of Chicago,
Chicago, IL 60637, USA
4Department of Earth Sciences, Syracuse University, Syracuse,
NY 13244,
USA
5Department of Geological Sciences, University of Florida, Gainesville,
FL 32611, USA
6GEOTOP, Université du Québec à Montréal, Montréal
QC, H3C 3P8, Canada
7Department of Earth and Planetary Sciences, Harvard University,
Cambridge, MA 02138, USA
8Department of Geography, Faculty of Engineering and Environment,
Northumbria University, Newcastle upon Tyne NE1 8ST, UK
9Center for Climate Systems Research at Columbia University, New York,
NY, USA
10NASA Goddard Institute for Space Studies, New York, NY, USA
Received: 16 Mar 2016 – Discussion started: 21 Mar 2016 – Revised: 22 Jun 2016 – Accepted: 23 Jun 2016 – Published: 13 Jul 2016
Abstract. The mid-Piacenzian is known as a period of relative warmth when compared to the present day. A comprehensive understanding of conditions during the Piacenzian serves as both a conceptual model and a source for boundary conditions as well as means of verification of global climate model experiments. In this paper we present the PRISM4 reconstruction, a paleoenvironmental reconstruction of the mid-Piacenzian ( ∼ 3 Ma) containing data for paleogeography, land and sea ice, sea-surface temperature, vegetation, soils, and lakes. Our retrodicted paleogeography takes into account glacial isostatic adjustments and changes in dynamic topography. Soils and lakes, both significant as land surface features, are introduced to the PRISM reconstruction for the first time. Sea-surface temperature and vegetation reconstructions are unchanged but now have confidence assessments. The PRISM4 reconstruction is being used as boundary condition data for the Pliocene Model Intercomparison Project Phase 2 (PlioMIP2) experiments.
Past intervals in Earth history provide unique windows into conditions much different than those observed today. We investigated the paleoenvironments of a past warm interval (~ 3 million years ago). Our reconstruction includes data sets for surface temperature, vegetation, soils, lakes, ice sheets, topography, and bathymetry. These data are being used along with global climate models to expand our understanding of the climate system and to help us prepare for future changes.
Past intervals in Earth history provide unique windows into conditions much different than those...
