Articles | Volume 18, issue 11
https://doi.org/10.5194/acp-18-8227-2018
© Author(s) 2018. This work is distributed under
the Creative Commons Attribution 4.0 License.
the Creative Commons Attribution 4.0 License.
https://doi.org/10.5194/acp-18-8227-2018
© Author(s) 2018. This work is distributed under
the Creative Commons Attribution 4.0 License.
the Creative Commons Attribution 4.0 License.
Surface impacts of the Quasi Biennial Oscillation
Lesley J. Gray
CORRESPONDING AUTHOR
National Centre for Atmospheric Sciences (NCAS), Department of Ocean,
Atmosphere and Planetary Physics, University of Oxford, Oxford, OX1 3PU,
UK
James A. Anstey
Canadian Centre for Climate Modelling and Analysis, Environment and
Climate Change Canada, University of Victoria, Victoria, V8W 2Y2, Canada
Yoshio Kawatani
Japan Agency for Marine-Earth Science and Technology, Yokohama,
236-0001, Japan
British Antarctic Survey, Cambridge, CB3 0ET, UK
Scott Osprey
National Centre for Atmospheric Sciences (NCAS), Department of Ocean,
Atmosphere and Planetary Physics, University of Oxford, Oxford, OX1 3PU,
UK
Verena Schenzinger
National Centre for Atmospheric Sciences (NCAS), Department of Ocean,
Atmosphere and Planetary Physics, University of Oxford, Oxford, OX1 3PU,
UK
Institute for Meteorology and Geophysics, University of Vienna, 1090
Vienna, Austria
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Short summary
A major phenomenon in the stratosphere is the Quasi Biennial Oscillation (QBO). Although a feature of the equatorial stratosphere, its influence extends to surface weather at both equatorial and mid latitudes. Improved knowledge of mechanisms of influence should help to improve weather forecasts. In this paper, QBO impacts at the surface are characterized and dominant mechanisms explored. Three pathways are identified, referred to as the tropical, subtropical and polar routes.
A major phenomenon in the stratosphere is the Quasi Biennial Oscillation (QBO). Although a...
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