1 Correction to: Clim Dyn (2016) 47:433–449 https://doi.org/10.1007/s00382-015-2846-0
Several mistakes occur in the original article that need to be notified.
In Table 1, the shallowness index (\( \upgamma \)) for the HadGEM2-ES model should be 44 ± 3, instead of 4 ± 3.
In Fig. 4a, the x-axis should start with the value 0 instead of − 20.
The convective drying index (∈c) is a dimensionless quantity (ratio). How-ever, an percent unit (%) was wrongly associated with ∈c in Figure 7 and Table 3.
Finally, the signs of ∈c in Table 3 are wrong. However, their values in Figure 7 remain exact. The updated table is available on page 2.
These corrections do not change the conclusions of the paper.
Model acronym | \( \upgamma \) (%) | ∈c (-) | Kmp (m2 s−1) | SHF, LHF, B (W m−2) | |||
---|---|---|---|---|---|---|---|
MIROC5 | 4 | 42 | 0.6 | 8.4 | 4.1 | 150 | 14.6 |
2.0 | 0.00 | − 0.10 | − 0.18 | 5.6 | 0.21 | ||
MRI-CGCM3 | 11 | 34 | 1.0 | 8.5 | 11.8 | 145 | 22.0 |
− 0.6 | − 0.02 | 0.20 | − 0.49 | 6.3 | − 0.05 | ||
MPI-ESM-LR | 15 | 70 | 2.1 | 6.4 | 12.9 | 139 | 22.6 |
− 1.9 | − 0.05 | 0.16 | − 0.50 | 5.9 | − 0.10 | ||
HadGEM2-ES | 17 | 46 | 0.7 | 8.1 | 10.7 | 150 | 21.2 |
1.1 | 0.02 | − 0.18 | − 0.28 | 5.2 | 0.09 | ||
IPSL-CM5A-LR | 21 | 65 | 2.3 | 5.8 | 18.0 | 135 | 27.4 |
− 2.8 | 0.00 | 0.28 | − 0.57 | 6.4 | − 0.12 | ||
IPSLA SCM | 69 | 3.1 | 3.9 | 12.8 | 119 | 21.1 | |
− 4.2 | 0.40 | 0.10 | − 0.64 | 3.7 | − 0.38 | ||
IPSLA SCM (no cv) | 40 | 0.0 | 3.2 | 11.4 | 111 | 19.1 | |
1.1 | 0.00 | − 0.02 | − 0.17 | 4.0 | 0.11 |
Table: Corrected Table 3 with updated ∈c values.
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Brient, F., Schneider, T., Tan, Z. et al. Correction to: Shallowness of tropical low clouds as a predictor of climate models’ response to warming. Clim Dyn 56, 2025 (2021). https://doi.org/10.1007/s00382-021-05675-2
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DOI: https://doi.org/10.1007/s00382-021-05675-2