Abstract
Several mistakes occur in the original article that need to be notified. In Table 1, the shallowness index ( γ ) 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 (ϵc) is a dimensionless quantity (ratio). How-ever, an percent unit (%) was wrongly associated with ϵc in Figure 7 and Table 3. Finally, the signs of ϵc 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. (Table presented.).
| Original language | English |
|---|---|
| Pages (from-to) | 2025 |
| Number of pages | 1 |
| Journal | Climate Dynamics |
| Volume | 56 |
| Issue number | 5-6 |
| DOIs |
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| Publication status | Published - 1 Mar 2021 |
UN SDGs
This output contributes to the following UN Sustainable Development Goals (SDGs)
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SDG 13 Climate Action
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Dive into the research topics of 'Correction to: Shallowness of tropical low clouds as a predictor of climate models’ response to warming (Climate Dynamics, (2016), 47, 1-2, (433-449), 10.1007/s00382-015-2846-0)'. Together they form a unique fingerprint.Cite this
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