Publication

Back to overview

Multidecadal variations of the effects of the Quasi-Biennial Oscillation on the climate system

Type of publication Peer-reviewed
Publikationsform Original article (peer-reviewed)
Publication date 2016
Author Brönnimann Stefan, Malik Abdul, Stickler Alexander, Wegmann Martin, Raible Christoph C., Muthers Stefan, Anet Julien, Rozanov Eugene, Schmutz Werner,
Project Future and Past Solar Influence on the Terrestrial Climate II
Show all

Original article (peer-reviewed)

Journal Atmospheric Chemistry and Physics
Volume (Issue) 16(24)
Page(s) 15529 - 15543
Title of proceedings Atmospheric Chemistry and Physics
DOI 10.5194/acp-16-15529-2016

Open Access

URL www.atmos-chem-phys.net/16/15529/2016/
Type of Open Access Publisher (Gold Open Access)

Abstract

Effects of the Quasi-Biennial Oscillation (QBO) on tropospheric climate are not always strong or they ap- pear only intermittently. Studying them requires long time series of both the QBO and climate variables, which has restricted previous studies to the past 30–50 years. Here we use the benefits of an existing QBO reconstruction back to 1908. We first investigate additional, newly digitized historical ob- servations of stratospheric winds to test the reconstruction. Then we use the QBO time series to analyse atmospheric data sets (reconstructions and reanalyses) as well as the re- sults of coupled ocean–atmosphere–chemistry climate model simulations that were forced with the reconstructed QBO. We investigate effects related to (1) tropical–extratropical inter- action in the stratosphere, wave–mean flow interaction and subsequent downward propagation, and (2) interaction be- tween deep tropical convection and stratospheric flow. We generally find weak connections, though some are statisti- cally significant over the 100-year period and consistent with model results. Apparent multidecadal variations in the con- nection between the QBO and the investigated climate responses are consistent with a small effect in the presence of large variability, with one exception: the imprint on the north- ern polar vortex, which is seen in recent reanalysis data, is not found in the period 1908–1957. Conversely, an imprint in Berlin surface air temperature is only found in 1908–1957 but not in the recent period. Likewise, in the model simulations both links tend to appear alternatingly, suggesting a more systematic modulation due to a shift in the circulation, for example. Over the Pacific warm pool, we find increased convection during easterly QBO, mainly in boreal winter in observation-based data as well as in the model simulations, with large variability. No QBO effects were found in the Indian monsoon strength or Atlantic hurricane frequency.
-