%0 Journal Article %1 hitchcock2016stratospheric %A Hitchcock, Peter %A Haynes, Peter H. %D 2016 %I American Geophysical Union (AGU) %J Geophysical Research Letters %K MyStratTropWork dynamics jet ssw stratosphere %N 22 %P 11,884--11,892 %R 10.1002/2016gl071372 %T Stratospheric control of planetary waves %U https://doi.org/10.1002%2F2016gl071372 %V 43 %X The equatorward shift of the zonal-mean midlatitude tropospheric jet following a stratospheric sudden warming in a comprehensive stratosphere-resolving model is found to be well quantified by the simple model of tropospheric eddy feedbacks proposed by Lorenz and Hartmann. This permits a decomposition of the shift into a component driven by the stratospheric anomalies and a component driven by tropospheric feedbacks. This is done by extending the simple model to include three effective forcing mechanisms by which the stratosphere may influence the tropospheric jet. These include 1) the zonally symmetric adjustments associated with the mean meridional circulation and the direct influence of the stratospheric anomalies on 2) the tropospheric synoptic-scale or 3) the tropospheric planetary-scale eddies. Although the anomalous tropospheric winds are primarily maintained against surface friction by the synoptic-scale eddies, this response can be entirely attributed to the eddy feedback term. The response of the planetary-scale eddies, in contrast, can be directly attributed to the stratosphere. The zonally symmetric tropospheric circulation associated with downward control is found to play little role in driving the tropospheric response. The prospects of applying this methodology to reanalysis data are also considered, but statistical limitations and the relatively weak projection of the vertically integrated composite wind anomalies onto the leading EOF preclude any conclusions from being drawn.

@article{hitchcock2016stratospheric, abstract = {The equatorward shift of the zonal-mean midlatitude tropospheric jet following a stratospheric sudden warming in a comprehensive stratosphere-resolving model is found to be well quantified by the simple model of tropospheric eddy feedbacks proposed by Lorenz and Hartmann. This permits a decomposition of the shift into a component driven by the stratospheric anomalies and a component driven by tropospheric feedbacks. This is done by extending the simple model to include three effective forcing mechanisms by which the stratosphere may influence the tropospheric jet. These include 1) the zonally symmetric adjustments associated with the mean meridional circulation and the direct influence of the stratospheric anomalies on 2) the tropospheric synoptic-scale or 3) the tropospheric planetary-scale eddies. Although the anomalous tropospheric winds are primarily maintained against surface friction by the synoptic-scale eddies, this response can be entirely attributed to the eddy feedback term. The response of the planetary-scale eddies, in contrast, can be directly attributed to the stratosphere. The zonally symmetric tropospheric circulation associated with downward control is found to play little role in driving the tropospheric response. The prospects of applying this methodology to reanalysis data are also considered, but statistical limitations and the relatively weak projection of the vertically integrated composite wind anomalies onto the leading EOF preclude any conclusions from being drawn.}, added-at = {2019-03-08T09:47:18.000+0100}, author = {Hitchcock, Peter and Haynes, Peter H.}, biburl = {https://www.bibsonomy.org/bibtex/249bf56035af8c6f8bedaaaf0dbb3c420/pbett}, doi = {10.1002/2016gl071372}, interhash = {60c38821bcfdf00536a03c672dd99b43}, intrahash = {49bf56035af8c6f8bedaaaf0dbb3c420}, journal = {Geophysical Research Letters}, keywords = {MyStratTropWork dynamics jet ssw stratosphere}, month = nov, number = 22, pages = {11,884--11,892}, publisher = {American Geophysical Union ({AGU})}, timestamp = {2019-03-08T09:47:18.000+0100}, title = {Stratospheric control of planetary waves}, url = {https://doi.org/10.1002%2F2016gl071372}, volume = 43, year = 2016 }