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Troposphere-Stratosphere Coupling in the Tropics: The Role of El Nino and the QBO

  • G. C. Reid
  • K. S. Gage
Conference paper
Part of the NATO ASI Series book series (volume 8)

Abstract

The chemical composition and dynamics of the tropical stratosphere are largely determined by forcing from the underlying troposphere,transmitted through the tropical tropopause. The properties of the tropopause region of the atmosphere are reviewed, with emphasis on the roles of Pacific sea-surface temperature variability in the El Niño mode and the stratospheric QBO as the principal factors that determine interannual variations.

Keywords

Convective Activity Meridional Circulation Lower Stratosphere Hadley Circulation Meridional Temperature Gradient 
These keywords were added by machine and not by the authors. This process is experimental and the keywords may be updated as the learning algorithm improves.

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Copyright information

© Springer-Verlag Berlin Heidelberg 1993

Authors and Affiliations

  • G. C. Reid
    • 1
  • K. S. Gage
    • 1
  1. 1.Aeronomy LaboratoryNational Oceanic and Atmospheric AdministrationBoulderUSA

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