Award Abstract # 1602967
Collaborative Research: P2C2--Late Holocene Climate: Natural or Anthropogenic?

NSF Org: AGS
Division of Atmospheric and Geospace Sciences
Recipient: RECTOR & VISITORS OF THE UNIVERSITY OF VIRGINIA
Initial Amendment Date: June 1, 2016
Latest Amendment Date: June 1, 2016
Award Number: 1602967
Award Instrument: Standard Grant
Program Manager: David Verardo
AGS
 Division of Atmospheric and Geospace Sciences
GEO
 Directorate for Geosciences
Start Date: June 1, 2016
End Date: May 31, 2019 (Estimated)
Total Intended Award Amount: $117,881.00
Total Awarded Amount to Date: $117,881.00
Funds Obligated to Date: FY 2016 = $117,881.00
History of Investigator:
  • William Ruddiman (Principal Investigator)
    wfr5c@virginia.edu
Recipient Sponsored Research Office: University of Virginia Main Campus
1001 EMMET ST N
CHARLOTTESVILLE
VA  US  22903-4833
(434)924-4270
Sponsor Congressional District: 05
Primary Place of Performance: The University of Virginia
291 McCormick Rd
Charlottesville
VA  US  22904-4123
Primary Place of Performance
Congressional District:
05
Unique Entity Identifier (UEI): JJG6HU8PA4S5
Parent UEI:
NSF Program(s): Paleoclimate
Primary Program Source: 01001617DB NSF RESEARCH & RELATED ACTIVIT
Program Reference Code(s): 7298, 7754, 8070
Program Element Code(s): 153000
Award Agency Code: 4900
Fund Agency Code: 4900
Assistance Listing Number(s): 47.050

ABSTRACT

This collaborative project generally aims to address a fundamental and yet unresolved question about Holocene climate which is: When did humans assume the "driver's seat" of the global climate system? Did it coincide with the advent of the Industrial Era, as traditionally believed, or did it instead occur many millennia ago with the emergence of agriculture?

The scientific community remains divided on whether carbon emissions released by early farming activities were large enough to explain the unprecedented rise in atmospheric greenhouse gas (GHG) concentrations during the late Holocene compared with declines in these climatic drivers during recent previous inter-glacial periods. This research will test the "Early Anthropogenic Hypothesis," which posits that anthropogenic global climate change was initiated by agriculture in the middle Holocene, by identifying the "fingerprint" of human influence on global climate during the past 6,000 years.

The project will capitalize on state-of-the-art earth system models to distinguish between the actual climatic evolution of the late Holocene and the hypothesized "natural" trajectory that would have been followed in the absence of human land clearance and greenhouse-gas overprints. To achieve this goal, a pair of 6,000-year long transient simulations will be run with the Community Earth System Model (CESM). In one experiment CESM will be driven by historical variations in orbital parameters, GHG concentrations, and regional land clearance, whereas the latter two forcings will differ in the counterpart experiment according to the hypothesized declines in carbon dioxide and methane and the associated global vegetation patterns compatible with "natural" climate evolution.

The Broader Impacts involve the potential for a unique and potentially transformative shift in the scientific understanding of human influence on global climate.

PUBLICATIONS PRODUCED AS A RESULT OF THIS RESEARCH

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S. Vavrus, F. he, J. Kutzbach, W. F. Ruddiman and P. C. Tzedakis "Glacial inception in marine isotope stage 19: An orbital analog for a natural Holocene climate." Nature Scientific Reports , v.8 , 2018 , p.Doi:10:10
W. F. Ruddiman "Geographic evidence of the early anthropogenic hypothesis" Anthropocene , v.20 , 2017 , p.4
W. F. Ruddiman "Reply to Anthropocene Working Group responses" Progress in Physical Geography , v.43 , 2019 , p.DOI: 10.1
W. F. Ruddiman "Three flaws in defining a formal "Anthropocene"" Progress in Physical Geography , v.42 , 2018 , p.451

PROJECT OUTCOMES REPORT

Disclaimer

This Project Outcomes Report for the General Public is displayed verbatim as submitted by the Principal Investigator (PI) for this award. Any opinions, findings, and conclusions or recommendations expressed in this Report are those of the PI and do not necessarily reflect the views of the National Science Foundation; NSF has not approved or endorsed its content.

My research, in collaboration with colleagues at the University of Wisconsin, focuses on comparing the observed climate of the last 7000 years against the way it would have developed in the absence of early anthropogenic alterations caused by agriculture. Beginning 7000-5000 years ago, early farming added substantial amounts of CO2 and methane to the atmosphere. Had this not occurred, climate would have cooled substantially, particularly at high latitudes, and small ice sheets would have begun to develop at high northern latitudes. 

One part of our approach (under my responsibility) has been to incorporate the wide range of multi-disciplinary research that has recently provided ground-truth evidence of agricultural transformations of Earth's surface, with resulting emissions of greenhouse gases. Deforestation emitted significant amounts of CO2 beginning 7000 years ago, and rice-paddy agriculture and tending of livestock emitted substantial methane after 5000 years ago. Several published papers by Ruddiman have synthesized these new developments.

My Wisconsin colleagues have used this ground-truth evidence to run two simulations on the NCAR CCSM4 climate model covering Holocene millennia. One simulation covers the observed evolution of climate (including the anthropogenic overprint), and one simulates the climate that would have developed withpout anthropogenic interference. Progress on this time-intensive modeling work has recently been slowed by an unexplained crash of the NCAR model that is now being examined.  

We have also published an influential paper on marine isotopic stage 19, the closest interglacial analog to the current interglaciation. During that interglaciation, CO2 fell to lower values close to those predicted by our early anthropogenic hypothesis, and ice cover developed in several far-northern regions, also as predicted.    

Our research has attracted wide attention from many scientists, who have published several dozen papers, some favoring and some opposing our hypothesis of early anthropogenic interference in the natural operation of the climate system. The resulting debate has also been widely covered in mainstream media.  

I (WFR) have also recently voiced my criticisms of the underway attempt by the Anthropogenic Working Group of the Subcommission of Quaternary Stratigraphy of the Geological Society of London to formalize the start of the "Anthropocene" at or around 1950. My basic counter-argument is that widespread alterations of Earth’s surface began 7000-5000 years ago. For example, full deforestation (reduced to modern levels) had occurred in most regions a millennium or more ago.

 

 


Last Modified: 05/31/2019
Modified by: William F Ruddiman

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