Award Abstract # 0630690
Collaborative Research: Global Aspects of Tropical Cyclogenesis

NSF Org: AGS
Division of Atmospheric and Geospace Sciences
Recipient: MASSACHUSETTS INSTITUTE OF TECHNOLOGY
Initial Amendment Date: September 26, 2006
Latest Amendment Date: September 26, 2006
Award Number: 0630690
Award Instrument: Standard Grant
Program Manager: Eric DeWeaver
edeweave@nsf.gov
 (703)292-8527
AGS
 Division of Atmospheric and Geospace Sciences
GEO
 Directorate for Geosciences
Start Date: October 1, 2006
End Date: September 30, 2009 (Estimated)
Total Intended Award Amount: $180,000.00
Total Awarded Amount to Date: $180,000.00
Funds Obligated to Date: FY 2006 = $180,000.00
History of Investigator:
  • Kerry Emanuel (Principal Investigator)
    emanuel@mit.edu
Recipient Sponsored Research Office: Massachusetts Institute of Technology
77 MASSACHUSETTS AVE
CAMBRIDGE
MA  US  02139-4301
(617)253-1000
Sponsor Congressional District: 07
Primary Place of Performance: Massachusetts Institute of Technology
77 MASSACHUSETTS AVE
CAMBRIDGE
MA  US  02139-4301
Primary Place of Performance
Congressional District:
07
Unique Entity Identifier (UEI): E2NYLCDML6V1
Parent UEI: E2NYLCDML6V1
NSF Program(s): Climate & Large-Scale Dynamics
Primary Program Source: app-0106 
Program Reference Code(s): 0000, OTHR
Program Element Code(s): 574000
Award Agency Code: 4900
Fund Agency Code: 4900
Assistance Listing Number(s): 47.050

ABSTRACT

Tropical cyclones (hurricanes) do not appear spontaneously in the tropical atmosphere; instead they must be triggered by a preexisting disturbance. It is hypothesized that these storms are subcritical instabilities of the tropical atmosphere. This implies that the strength of the disturbance necessary to trigger a hurricane depends on the background state of the tropical atmosphere and ocean, and that, at least in theory, hurricanes could appear spontaneously in a different climate, one with instability parameters that exceed a critical point.

The hypothesis of subcritical instability will be explored using a high-resolution numerical model to map out the instability diagram for tropical cyclogenesis and to reveal physical processes underlying the structure of this diagram. Physical insights from these experiments, together with observational data and experiments with a more idealized model, will be used to develop and refine a cyclogenesis index. Ultimately such an index can provide information about the frequency with which hurricanes form in different climates.

Broader impacts of this research include training a graduate student and a post-doctoral researcher, as well as developing understanding and tools that could lead to improved predictions of how tropical cyclone activity will change as climate changes, either naturally or due to human influence.

PUBLICATIONS PRODUCED AS A RESULT OF THIS RESEARCH

Note:  When clicking on a Digital Object Identifier (DOI) number, you will be taken to an external site maintained by the publisher. Some full text articles may not yet be available without a charge during the embargo (administrative interval).

Some links on this page may take you to non-federal websites. Their policies may differ from this site.

Boos, W. R., and K. A. Emanuel "Wind?evaporation feedback and abrupt seasonal transitions of weak, axisymmetric Hadley circulations" J. Atmos. Sci. , v.65 , 2008 , p.2194
Camargo, S. J., A. H. Sobel, A. G. Barnston, and K. A. Emanuel "Tropical cyclone genesis potential index in climate models" Tellus , v.59 , 2007 , p.428
Dean, L; Emanuel, KA; Chavas, DR "On the size distribution of Atlantic tropical cyclones" GEOPHYSICAL RESEARCH LETTERS , v.36 , 2009 View record at Web of Science 10.1029/2009GL03905
Nolan, DQ; Rappin, ED; Emanuel, KA "Could random convection form hurricanes in a warmer world?" BULLETIN OF THE AMERICAN METEOROLOGICAL SOCIETY , v.87 , 2006 , p.559 View record at Web of Science

Please report errors in award information by writing to: awardsearch@nsf.gov.

Print this page

Back to Top of page