Award Abstract # 2103092
Collaborative Research: P2C2--El Niño Southern Oscillation (ENSO) Variability Changes during Abrupt Climate Events

NSF Org: AGS
Division of Atmospheric and Geospace Sciences
Recipient: UNIVERSITY OF TEXAS AT AUSTIN
Initial Amendment Date: April 16, 2021
Latest Amendment Date: August 3, 2021
Award Number: 2103092
Award Instrument: Continuing Grant
Program Manager: Mea S. Cook
mcook@nsf.gov
 (703)292-7306
AGS
 Division of Atmospheric and Geospace Sciences
GEO
 Directorate for Geosciences
Start Date: May 1, 2021
End Date: April 30, 2025 (Estimated)
Total Intended Award Amount: $1,150,800.00
Total Awarded Amount to Date: $1,150,800.00
Funds Obligated to Date: FY 2021 = $1,150,800.00
History of Investigator:
  • Judson Partin (Principal Investigator)
    jpartin@ig.utexas.edu
  • Yuko Okumura (Co-Principal Investigator)
Recipient Sponsored Research Office: University of Texas at Austin
110 INNER CAMPUS DR
AUSTIN
TX  US  78712-1139
(512)471-6424
Sponsor Congressional District: 25
Primary Place of Performance: University of Texas Institute for Geophysics
10100 Burnet Rd., Bldg. 196/ROC
Austin
TX  US  78758-4445
Primary Place of Performance
Congressional District:
37
Unique Entity Identifier (UEI): V6AFQPN18437
Parent UEI:
NSF Program(s): Paleoclimate
Primary Program Source: 01002122DB NSF RESEARCH & RELATED ACTIVIT
01002223DB NSF RESEARCH & RELATED ACTIVIT

01002324DB NSF RESEARCH & RELATED ACTIVIT
Program Reference Code(s): 8070, 7754
Program Element Code(s): 153000
Award Agency Code: 4900
Fund Agency Code: 4900
Assistance Listing Number(s): 47.050

ABSTRACT

The research team aims to reconstruct changes in variability of the El Nino/Southern Oscillation (ENSO) during the last deglacial period by measuring coral delta O-18 on previously collected samples from Vanuatu in the tropical southwestern Pacific Ocean. Modern coral delta O-18records from Vanuatu and pseudoproxy experiments show a high degree of skill in capturing changes in ENSO variability, providing confidence that the resulting records can be used to reconstruct past ENSO variability. The researchers will compare the reconstructions to climate model output of ENSO during previous glacial times when Atlantic Meridional Overturning Circulation (AMOC) was both vigorous and sluggish.

The research team?s current hypotheses, based on climate model output, is that ENSO was reduced during glacial times, relative to modern, and that ENSO was more active when AMOC was shutdown, relative to contemporaneous glacial times when AMOC was active.

The team will conduct hosing model experiments under glacial boundary conditions to test the sensitivity of ENSO and AMOC changes to background conditions. The research will also investigate how non-stationarity of ENSO may affect the skills of Vanuatu corals by using an ensemble of climate models run under different climate boundary conditions.

The project may help shed light on the sensitivity of ENSO to external forcing, a highly critical issue given that climate models used for future climate projections do not agree if ENSO will strengthen or weaken as the Earth warms.

The potential Broader Impacts include a deeper understanding of ENSO variability, development of a new drilling system for field research, involvement of graduate and undergraduate students in the research including undergraduates at a primarily undergraduate teaching institution.

This award reflects NSF's statutory mission and has been deemed worthy of support through evaluation using the Foundation's intellectual merit and broader impacts review criteria.

PUBLICATIONS PRODUCED AS A RESULT OF THIS RESEARCH

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Lawman, Allison E. and Di Nezio, Pedro N. and Partin, Judson W. and Dee, Sylvia G. and Thirumalai, Kaustubh and Quinn, Terrence M. "Unraveling forced responses of extreme El Niño variability over the Holocene" Science Advances , v.8 , 2022 https://doi.org/10.1126/sciadv.abm4313 Citation Details

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