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A new perspective on the dynamical link between the stratosphere and troposphere

A new perspective on the dynamical link between the stratosphere and troposphere Atmospheric processes of tropospheric origin can perturb the stratosphere, but direct feedback in the opposite direction is usually assumed to be negligible, despite the troposphere's sensitivity to changes in the release of wave activity into the stratosphere 1,2,3 . Here, however, we present evidence that such a feedback exists and can be significant. We find that if the wintertime Arctic polar stratospheric vortex is distorted, either by waves propagating upward from the troposphere 4 or by eastward-travelling stratospheric waves 5 , 6 , then there is a concomitant redistribution of stratospheric potential vorticity which induces perturbations in keymeteorological fields in the upper troposphere. The feedback is large despite the much greater mass of the troposphere: it can account for up to half of the geopotential height anomaly at thetropopause. Although the relative strength ofthefeedback is partly due to a cancellation 7 between contributions to these anomalies from lower altitudes, our results imply that stratospheric dynamics and its feedback on the troposphere are more significant for climate modelling and data assimilation than was previously assumed. http://www.deepdyve.com/assets/images/DeepDyve-Logo-lg.png Nature Springer Journals

A new perspective on the dynamical link between the stratosphere and troposphere

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References (26)

Publisher
Springer Journals
Copyright
Copyright © 1998 by Macmillan Magazines Ltd.
Subject
Science, Humanities and Social Sciences, multidisciplinary; Science, Humanities and Social Sciences, multidisciplinary; Science, multidisciplinary
ISSN
0028-0836
eISSN
1476-4687
DOI
10.1038/35112
Publisher site
See Article on Publisher Site

Abstract

Atmospheric processes of tropospheric origin can perturb the stratosphere, but direct feedback in the opposite direction is usually assumed to be negligible, despite the troposphere's sensitivity to changes in the release of wave activity into the stratosphere 1,2,3 . Here, however, we present evidence that such a feedback exists and can be significant. We find that if the wintertime Arctic polar stratospheric vortex is distorted, either by waves propagating upward from the troposphere 4 or by eastward-travelling stratospheric waves 5 , 6 , then there is a concomitant redistribution of stratospheric potential vorticity which induces perturbations in keymeteorological fields in the upper troposphere. The feedback is large despite the much greater mass of the troposphere: it can account for up to half of the geopotential height anomaly at thetropopause. Although the relative strength ofthefeedback is partly due to a cancellation 7 between contributions to these anomalies from lower altitudes, our results imply that stratospheric dynamics and its feedback on the troposphere are more significant for climate modelling and data assimilation than was previously assumed.

Journal

Nature – Springer Journals

Published: Jan 29, 1998

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