Award Abstract # 0902844
Collaborative Research: P2C2--Understanding the Role of a High-Latitude Convective Cloud Feedback in Equable and Future Climate Dynamics

NSF Org: AGS
Division of Atmospheric and Geospace Sciences
Recipient: PRESIDENT AND FELLOWS OF HARVARD COLLEGE
Initial Amendment Date: June 9, 2009
Latest Amendment Date: May 26, 2011
Award Number: 0902844
Award Instrument: Standard Grant
Program Manager: David Verardo
AGS
 Division of Atmospheric and Geospace Sciences
GEO
 Directorate for Geosciences
Start Date: June 15, 2009
End Date: May 31, 2013 (Estimated)
Total Intended Award Amount: $461,147.00
Total Awarded Amount to Date: $461,147.00
Funds Obligated to Date: FY 2009 = $461,147.00
ARRA Amount: $461,147.00
History of Investigator:
  • Eli Tziperman (Principal Investigator)
    eli@eps.harvard.edu
Recipient Sponsored Research Office: Harvard University
1033 MASSACHUSETTS AVE STE 3
CAMBRIDGE
MA  US  02138-5366
(617)495-5501
Sponsor Congressional District: 05
Primary Place of Performance: Harvard University
1033 MASSACHUSETTS AVE STE 3
CAMBRIDGE
MA  US  02138-5366
Primary Place of Performance
Congressional District:
05
Unique Entity Identifier (UEI): LN53LCFJFL45
Parent UEI:
NSF Program(s): Paleoclimate
Primary Program Source: 01R00910DB RRA RECOVERY ACT
Program Reference Code(s): 1304, 6890, EGCH
Program Element Code(s): 153000
Award Agency Code: 4900
Fund Agency Code: 4900
Assistance Listing Number(s): 47.050

ABSTRACT

Funding is provided to investigate equator-to-pole temperature differences and high-latitude seasonality during the equable climate of the Eocene Period when both were much smaller than they are today. These circumstances are difficult to explain within the framework of the current understanding of climate dynamics.

The researchers seek to: 1) understand what factors control the critical carbon dioxide level at which the convective cloud feedback activates and the magnitude of the surface warming the feedback can produce; 2) determine the ability of convective cloud feedback to provide warming in continental interiors as well as over ocean, consistent with Eocene fossil and proxy observations; 3) constrain the convective cloud feedback using modern observations; and 4) investigate the possible implications of the convective cloud feedback for future climate.

The broader impacts are primarily the support of a postdoctoral scholar and graduate student.

This award is funded under the American Recovery and Reinvestment Act of 2009 (Public Law 111-5).

PUBLICATIONS PRODUCED AS A RESULT OF THIS RESEARCH

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(Showing: 1 - 10 of 23)
Abbot, D. S. and Halevy, I. "Dust Aerosol Important for Snowball Earth Deglaciation." J. Climate , v.23 , 2010 , p.4121?4132 10.1175/2010JCLI3378.1
Abbot, D. S. and Pierrehumbert, R. T. "Mudball: Surface dust and Snowball Earth deglaciation." J. Geophys. Res. , v.115 , 2010 , p.10.1029/2 10.1029/2009JD012007
Abbot, D. S., Eisenman, I., and Pierrehumbert, R. T. "The importance of ice vertical resolution for Snowball climate and deglaciation." J. Climate , v.23 , 2010 , p.6100?6109
Abbot, DS; Eisenman, I; Pierrehumbert, RT "The Importance of Ice Vertical Resolution for Snowball Climate and Deglaciation" JOURNAL OF CLIMATE , v.23 , 2010 , p.6100 View record at Web of Science 10.1175/2010JCLI3693.
Abbot, DS; Halevy, I "Dust Aerosol Important for Snowball Earth Deglaciation" JOURNAL OF CLIMATE , v.23 , 2010 , p.4121 View record at Web of Science 10.1175/2010JCLI3378.
Abbot, DS; Pierrehumbert, RT "Mudball: Surface dust and Snowball Earth deglaciation" JOURNAL OF GEOPHYSICAL RESEARCH-ATMOSPHERES , v.115 , 2010 View record at Web of Science 10.1029/2009JD01200
Arnold, N., Kuang, Z., and Tziperman, E. "Enhanced MJO-like variability at high SST." J. Climate , v.26 , 2013 , p.988?1001
Arnold, NP; Tziperman, E; Farrell, B "Abrupt Transition to Strong Superrotation Driven by Equatorial Wave Resonance in an Idealized GCM" JOURNAL OF THE ATMOSPHERIC SCIENCES , v.69 , 2012 , p.626 View record at Web of Science 10.1175/JAS-D-11-0136.
Arnold, N., Tziperman, E., and Farrell, B. F. "Abrupt transition to strong superrota- tion driven by equatorial wave resonance in an idealized GCM." J. Atmos. Sci. , v.69 , 2012 , p.626?640
Ashkenazy, Y., Eisenman, I., Gildor, H., and Tziperman, E. "The effect of milankovitch variations in insolation on equatorial seasonality." Journal of Climate , v.23 , 2010 , p.613
Ashkenazy, Y., Eisenman, I., Gildor, H., and Tziperman, E. "The effect of Milankovitch variations in insolation on equatorial seasonality." j climate , v.23 , 2010 , p.6133?6142
(Showing: 1 - 10 of 23)

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