Climate Dynamics

, Volume 50, Issue 7–8, pp 2813–2827 | Cite as

A warming tropical central Pacific dries the lower stratosphere

  • Qinghua Ding
  • Qiang Fu


The amount of water vapor in the tropical lower stratosphere (TLS), which has an important influence on the radiative energy budget of the climate system, is modulated by the temperature variability of the tropical tropopause layer (TTL). The TTL temperature variability is caused by a complex combination of the stratospheric quasi-biennial oscillation (QBO), tropospheric convective processes in the tropics, and the Brewer–Dobson circulation (BDC) driven by mid-latitude and subtropical atmospheric waves. In 2000, the TLS water vapor amount exhibited a stepwise transition to a dry phase, apparently caused by a change in the BDC. In this study, we present observational and modeling evidence that the epochal change of water vapor between the periods of 1992–2000 and 2001–2005 was also partly caused by a concurrent sea surface temperature (SST) warming in the tropical central Pacific. This SST warming cools the TTL above by enhancing the equatorial wave-induced upward motion near the tropopause, which consequently reduces the amount of water vapor entering the stratosphere. The QBO affects the TLS water vapor primarily on inter-annual timescales, whereas a classical El Niño southern oscillation (ENSO) event has small effect on tropical mean TLS water vapor because its responses are longitudinally out of phase. This study suggests that the tropical central Pacific SST is another driver of TLS water vapor variability on inter-decadal timescales and the tropical SST changes could contribute to about 30% of the step-wise drop of the lower stratospheric water vapor from 1992–2000 to 2001–2005.


Troposphere–stratosphere interaction Tropical central Pacific SST Stratospheric water vapor change Interdecadal variability 



We thank Profs. J. M. Wallace and Dr. S. Po-Chedley for helpful discussions and comments on the manuscript. We thank the Max Planck Institute for Meteorology for making the ECHAM5 available. This work was supported by NASA Grants NNX13AN49G and NNX16AO95G. Q. Ding is grateful for funding from the National Science Foundation through grant NSF PLR 1443144.


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Copyright information

© Springer-Verlag GmbH Germany 2017

Authors and Affiliations

  1. 1.Department of GeographyUniversity of California, Santa BarbaraSanta BarbaraUSA
  2. 2.Department of Atmospheric SciencesUniversity of WashingtonSeattleUSA

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