CORRIGENDUM

Clémence Macron Centre de Recherches de Climatologie, CNRS/Université de Bourgogne, Dijon, France

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Benjamin Pohl Centre de Recherches de Climatologie, CNRS/Université de Bourgogne, Dijon, France

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Yves Richard Centre de Recherches de Climatologie, CNRS/Université de Bourgogne, Dijon, France

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Miloud Bessafi Laboratoire d’Energétique, d’Electronique et Procédés, Université de la Réunion, Réunion, France

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Corresponding author address: Clémence Macron, Centre de Recherches de Climatologie, CNRS/Université de Bourgogne, 6 Bd. Gabriel, 21000 Dijon, France. E-mail: clemence.macron@u-bourgogne.fr

Corresponding author address: Clémence Macron, Centre de Recherches de Climatologie, CNRS/Université de Bourgogne, 6 Bd. Gabriel, 21000 Dijon, France. E-mail: clemence.macron@u-bourgogne.fr

Figure 3 in Macron et al. (2014) contains an error (a curve showing divergence instead of convergence anomalies).

Fig. 3.
Fig. 3.

Longitudinal profiles of OLR (blue), 200-hPa ZDEF (blue dots), and wind convergence at 200 hPa (red) anomalies for classes 5, 6, and 7, averaged over the 36°–24°S latitudinal band. Blue (orange) shadings denote regions of enhanced (suppressed) convection.

Citation: Journal of Climate 27, 13; 10.1175/JCLI-D-14-00319.1

The correct figure and comments appear below as they should have appeared.

Regions of enhanced (reduced) convection exhibit negative convergence (divergence) anomalies at 200 hPa and vice versa at 850 hPa (not shown), indicating a consistent baroclinic structure favoring deep convection.

We regret any inconvenience this error may have caused.

REFERENCE

Macron, C., B. Pohl, Y. Richard, and M. Bessafi, 2014: How do tropical temperate troughs form and develop over southern Africa? J. Climate, 27, 16331647, doi:10.1175/JCLI-D-13-00175.1.

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  • Macron, C., B. Pohl, Y. Richard, and M. Bessafi, 2014: How do tropical temperate troughs form and develop over southern Africa? J. Climate, 27, 16331647, doi:10.1175/JCLI-D-13-00175.1.

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  • Fig. 3.

    Longitudinal profiles of OLR (blue), 200-hPa ZDEF (blue dots), and wind convergence at 200 hPa (red) anomalies for classes 5, 6, and 7, averaged over the 36°–24°S latitudinal band. Blue (orange) shadings denote regions of enhanced (suppressed) convection.

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