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AGU: Geophysical Research Letters

 

Keywords

  • satellite data
  • stratospheric sudden warming

Index Terms

  • Atmospheric Processes: Middle atmosphere dynamics
  • Atmospheric Processes: Remote sensing
  • Atmospheric Composition and Structure: Middle atmosphere: constituent transport and chemistry
  • Atmospheric Processes: Polar meteorology

Abstract

Aura Microwave Limb Sounder observations of dynamics and transport during the record-breaking 2009 Arctic stratospheric major warming

Gloria L. Manney

Jet Propulsion Laboratory, California Institute of Technology, Pasadena, California, USA

Michael J. Schwartz

Jet Propulsion Laboratory, California Institute of Technology, Pasadena, California, USA

Kirstin Krüger

Leibniz Institute for Marine Sciences at Kiel University, Kiel, Germany

Michelle L. Santee

Jet Propulsion Laboratory, California Institute of Technology, Pasadena, California, USA

Steven Pawson

NASA Goddard Space Flight Center, Greenbelt, Maryland, USA

Jae N. Lee

Jet Propulsion Laboratory, California Institute of Technology, Pasadena, California, USA

William H. Daffer

Jet Propulsion Laboratory, California Institute of Technology, Pasadena, California, USA

Ryan A. Fuller

Jet Propulsion Laboratory, California Institute of Technology, Pasadena, California, USA

Nathaniel J. Livesey

Jet Propulsion Laboratory, California Institute of Technology, Pasadena, California, USA

A major stratospheric sudden warming (SSW) in January 2009 was the strongest and most prolonged on record. Aura Microwave Limb Sounder (MLS) observations are used to provide an overview of dynamics and transport during the 2009 SSW, and to compare with the intense, long-lasting SSW in January 2006. The Arctic polar vortex split during the 2009 SSW, whereas the 2006 SSW was a vortex displacement event. Winds reversed to easterly more rapidly and reverted to westerly more slowly in 2009 than in 2006. More mixing of trace gases out of the vortex during the decay of the vortex fragments, and less before the fulfillment of major SSW criteria, was seen in 2009 than in 2006; persistent well-defined fragments of vortex and anticyclone air were more prevalent in 2009. The 2009 SSW had a more profound impact on the lower stratosphere than any previously observed SSW, with no significant recovery of the vortex in that region. The stratopause breakdown and subsequent reformation at very high altitude, accompanied by enhanced descent into a rapidly strengthening upper stratospheric vortex, were similar in 2009 and 2006. Many differences between 2006 and 2009 appear to be related to the different character of the SSWs in the two years.

Received 10 April 2009; accepted 27 May 2009; published 27 June 2009.

Citation: Manney, G. L., M. J. Schwartz, K. Krüger, M. L. Santee, S. Pawson, J. N. Lee, W. H. Daffer, R. A. Fuller, and N. J. Livesey (2009), Aura Microwave Limb Sounder observations of dynamics and transport during the record-breaking 2009 Arctic stratospheric major warming, Geophys. Res. Lett., 36, L12815, doi:10.1029/2009GL038586.

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