Award Abstract # 1247464
Stratosphere-troposphere Coupling during Anticyclogenesis

NSF Org: AGS
Division of Atmospheric and Geospace Sciences
Recipient: CORNELL UNIVERSITY
Initial Amendment Date: April 10, 2013
Latest Amendment Date: February 22, 2017
Award Number: 1247464
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: April 1, 2013
End Date: March 31, 2018 (Estimated)
Total Intended Award Amount: $448,657.00
Total Awarded Amount to Date: $448,657.00
Funds Obligated to Date: FY 2013 = $448,657.00
History of Investigator:
  • Stephen Colucci (Principal Investigator)
    sjc25@cornell.edu
Recipient Sponsored Research Office: Cornell University
341 PINE TREE RD
ITHACA
NY  US  14850-2820
(607)255-5014
Sponsor Congressional District: 19
Primary Place of Performance: Cornell University
NY  US  14850-2820
Primary Place of Performance
Congressional District:
19
Unique Entity Identifier (UEI): G56PUALJ3KT5
Parent UEI:
NSF Program(s): Climate & Large-Scale Dynamics
Primary Program Source: 01001314DB NSF RESEARCH & RELATED ACTIVIT
Program Reference Code(s): OTHR
Program Element Code(s): 574000
Award Agency Code: 4900
Fund Agency Code: 4900
Assistance Listing Number(s): 47.050

ABSTRACT

This project seeks to understand how tropospheric blocking events lead to stratospheric sudden stratospheric warmings (SSWs). Previous research has shown a statistically significant relationship in which most SSWs are preceded by blocking events, yet the majority of blocking events are not followed SSWs. The goal of this research is to determine what factors cause some blocks to perturb the stratosphere while others do not. The research is conducted through a combination of dynamical diagnosis of reanalysis datasets and numerical experiments conducted with an idealized atmospheric model.

The research topic is of practical importance as well as scientific interest, as SSWs are known to affect subsequent weather and are particularly associated with cold air outbreaks. Results of this research may thus be of interest for long-range weather forecasting. In addition, the project supports two graduate students, thereby providing for the next generation of researchers in this area.

PUBLICATIONS PRODUCED AS A RESULT OF THIS RESEARCH

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Stephen J. Colucci and Michael E. Kelleher "Diagnostic comparison of tropospheric blocking events with and without stratospheric warming" Journal of the Atmospheric Sciences , v.72 , 2015 , p.2227
Stephen J. Colucci and Michael E. Kelleher "Diagnostic Comparison of Tropospheric Blocking with and without Sudden Stratospheric Warming" Journal of the Atmospheric Sciences , 2015
Stephen J. Colucci and Thomas S. Ehrmann "Synoptic-dynamic climatology of the Aleutian High" Journal of the Atmospheric Sciences , v.75 , 2018 , p.1271

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.

The purpose of the project was to investigate the relationship between anticyclones (clockwise spinning high-pressure systems) in the lower atmosphere (0 - 30 kilometers above sea-level) and the stratospheric polar vortex (a high-latitude, counterclockwise spinning low pressure system 25 - 30 kilometers above sea-level) in Northern Hemisphere winter seasons.  Disturbances to the polar vortex, such as its splitting into two or more vortices or its displacement away from the North Pole, can be followed in time by abnormally cold weather at the earth's surface.  These disturbances were found on average to be preceded in time by the development of an anticyclone over the Aleutian Islands 30 kilometers above sea level, and by the development of unusually strong anticyclones ("blocking highs") closer to sea level.  The mechanism connecting these anticyclones with the disturbed polar vortex was found to be an abnormal flow of warm air from low to high latitudes.  In addition, abnormally cold air near sea-level can help disturb the polar vortex, setting the stage for further cold weather conditions near sea level.

      These discoveries were made by the principal investigator and his two graduate students, one of whom earned a Ph.D. degree and is now employed as a research scientist while the other is completing his Ph.D.   This latter student also supervised an undergraduate student on aspects of the project, exposing that student to research methods and discovery.  These students and the investigator published their findings in scholarly journals read by other students and scientists, and presented their work to audiences at scientific conferences.  Finally, the research methods used in the project were introduced to other graduate and undergraduate students in the courses taught by the investigator.


Last Modified: 05/30/2018
Modified by: Stephen J Colucci

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