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Cited by 386

The DOI matches its Crossref record; 29 of the 29 references it cites were found in a registry or an index.

The Influence of Sea Surface Temperatures on the Northern Winter Stratosphere: Ensemble Simulations with the MAECHAM5 Model

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Manzini, E., Giorgetta, M. A., Esch, M., Kornblueh, L., Roeckner, E.·2006·Journal of Climate

Abstract

The role of interannual variations in sea surface temperatures (SSTs) on the Northern Hemisphere winter polar stratospheric circulation is addressed by means of an ensemble of nine simulations performed with the middle atmosphere configuration of the ECHAM5 model forced with observed SSTs during the 20-yr period from 1980 to 1999. Results are compared to the 40-yr ECMWF Re-Analysis (ERA-40). Three aspects have been considered: the influence of the interannual SST variations on the climatological mean state, the response to El Niño–Southern Oscillation (ENSO) events, and the influence on systematic temperature changes. The strongest influence of SST variations has been found for the warm ENSO events considered. Namely, it has been found that the large-scale pattern associated with the extratropical tropospheric response to the ENSO phenomenon during northern winter enhances the forcing and the vertical propagation into the stratosphere of the quasi-stationary planetary waves emerging from the troposphere. This enhanced planetary wave disturbance thereafter results in a polar warming of a few degrees in the lower stratosphere in late winter and early spring. Consequently, the polar vortex is weakened, and the warm ENSO influence clearly emerges also in the zonal-mean flow. In contrast, the cold ENSO events considered do not appear to have an influence distinguishable from that of internal variability. It is also not straightforward to deduce the influence of the SSTs on the climatological mean state from the simulations performed, because the simulated internal variability of the stratosphere is large, a realistic feature. Moreover, the results of the ensemble of simulations provide weak to negligible evidence for the possibility that SST variations during the two decades considered are substantially contributing to changes in the polar temperature in the winter lower stratosphere.

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Metadata

Authors
Manzini, E., Giorgetta, M. A., Esch, M., Kornblueh, L., & Roeckner, E.
Venue
Journal of Climate
Published
2006-08-15
Volume
19
Issue
16
Pages
3863-3881
ISSN
  • 0894-8755 (ISSN-L)
  • 1520-0442
OpenAlex
W2079985720
Cited by
386
References
29
FWCI
11.33
Type
journal article
Language
en
Open access
bronze

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