Research Article
Brewer–Dobson Circulation: Recent-Past and Near-Future Trends Simulated by Chemistry-Climate Models
Table 1
CCMVal-2 models used in this study
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| Model name | Resolution | Vertical layers | Model top | REF-B1 (1960–2000) | REF-B2 (2001–2050) |
| AMTRAC3 | | 48 | 0.0017 hPa | 1 | | CAM3.5 | | 31 | 0.10 hPa | 1 | 1 | CCSRNIES | | 34 | 0.01 hPa | 1 | 1 | CMAM | | 71 | 0.0006 hPa | 3 | 3 | CNRM-ACM | | 31 | 0.10 hPa | 2 | 1 | E39CA | | 39 | 10 hPa | 1 | | EMAC | | 31 | 0.10 hPa | 1 | | GEOSCCM | | 55 | 0.01 hPa | 1 | 1 | LMDZrepro | | 50 | 0.07 hPa | 3 | | MRI | | 68 | 0.01 hPa | 4 | 2 | Niwa-SOCOL | | 31 | 0.1 hPa | 1 | | SOCOL | | 39 | 0.1 hPa | 3 | 3 | ULAQ | | 26 | 0.04 hPa | 1 | | UMSLIMCAT | | 64 | 0.01 hPa | 1 | 1 | UMUKCA-METO | | 31 | 10 hPa | 1 | 1 | WACCM | | 66 | hPa | 4 | 3 |
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The numbers in the fourth and fifth columns represent the number of ensemble members; more details are available in Morgenstern et al. [28].
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