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The DOI matches its Crossref record; 33 of the 33 references it cites were found in a registry or an index.

On the lack of stratospheric dynamical variability in low‐top versions of the CMIP5 models

Open access
Charlton‐Perez, Andrew J., Baldwin, Mark P., Birner, Thomas, Black, Robert X., Butler, Amy H., Calvo, Natalia, Davis, Nicholas A., Gerber, Edwin P., Gillett, Nathan, Hardiman, Steven, Kim, Junsu, Krüger, Kirstin, Lee, Yun‐Young, Manzini, Elisa, McDaniel, Brent A., Polvani, Lorenzo, Reichler, Thomas, Shaw, Tiffany A., Sigmond, Michael, Son, Seok‐Woo, Toohey, Matthew, Wilcox, Laura, Yoden, Shigeo, Christiansen, Bo, Lott, François, Shindell, Drew, Yukimoto, Seiji, Watanabe, Shingo·2013·Journal of Geophysical Research: Atmospheres

Abstract

We describe the main differences in simulations of stratospheric climate and variability by models within the fifth Coupled Model Intercomparison Project (CMIP5) that have a model top above the stratopause and relatively fine stratospheric vertical resolution (high‐top), and those that have a model top below the stratopause (low‐top). Although the simulation of mean stratospheric climate by the two model ensembles is similar, the low‐top model ensemble has very weak stratospheric variability on daily and interannual time scales. The frequency of major sudden stratospheric warming events is strongly underestimated by the low‐top models with less than half the frequency of events observed in the reanalysis data and high‐top models. The lack of stratospheric variability in the low‐top models affects their stratosphere‐troposphere coupling, resulting in short‐lived anomalies in the Northern Annular Mode, which do not produce long‐lasting tropospheric impacts, as seen in observations. The lack of stratospheric variability, however, does not appear to have any impact on the ability of the low‐top models to reproduce past stratospheric temperature trends. We find little improvement in the simulation of decadal variability for the high‐top models compared to the low‐top, which is likely related to the fact that neither ensemble produces a realistic dynamical response to volcanic eruptions.

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Metadata

Authors
Charlton‐Perez, A. J., Baldwin, M. P., Birner, T., Black, R. X., Butler, A. H., Calvo, N., Davis, N. A., Gerber, E. P., Gillett, N., Hardiman, S., Kim, J., Krüger, K., Lee, Y., Manzini, E., McDaniel, B. A., Polvani, L., Reichler, T., Shaw, T. A., Sigmond, M., Son, S., Toohey, M., Wilcox, L., Yoden, S., Christiansen, B., Lott, F., Shindell, D., Yukimoto, S., & Watanabe, S.
Venue
Journal of Geophysical Research: Atmospheres
Published
2013-03-27
Volume
118
Issue
6
Pages
2494-2505
ISSN
  • 0148-0227 (ISSN-L)
  • 2169-897X
  • 2169-8996
OpenAlex
W2147752502
Cited by
331
References
33
FWCI
21.20
Type
journal article
Language
en
Open access
bronze

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CoChat. (2026). Citation check: On the lack of stratospheric dynamical variability in low‐top versions of the CMIP5 models. https://app.cochat.ai/papers/10.1002/jgrd.50125
The paper
Charlton‐Perez, A. J., Baldwin, M. P., Birner, T., Black, R. X., Butler, A. H., Calvo, N., Davis, N. A., Gerber, E. P., Gillett, N., Hardiman, S., Kim, J., Krüger, K., Lee, Y., Manzini, E., McDaniel, B. A., Polvani, L., Reichler, T., Shaw, T. A., Sigmond, M., . . . Watanabe, S. (2013). On the lack of stratospheric dynamical variability in low‐top versions of the CMIP5 models. Journal of Geophysical Research: Atmospheres. https://doi.org/10.1002/jgrd.50125

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