Editorial Type:
Corrigendum
Article Type:
Correction

CORRIGENDUM

Andréa S. Taschetto Climate Change Research Centre and ARC Centre of Excellence for Climate System Science, University of New South Wales, Sydney, New South Wales, Australia

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Alex Sen Gupta Climate Change Research Centre and ARC Centre of Excellence for Climate System Science, University of New South Wales, Sydney, New South Wales, Australia

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Harry H. Hendon Centre for Australian Weather and Climate Research, Bureau of Meteorology, Melbourne, Victoria, Australia

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Caroline C. Ummenhofer Department of Physical Oceanography, Woods Hole Oceanographic Institution, Woods Hole, Massachusetts

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Matthew H. England Climate Change Research Centre and ARC Centre of Excellence for Climate System Science, University of New South Wales, Sydney, New South Wales, Australia

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Print Publication:
01 Dec 2013
DOI:
https://doi.org/10.1175/JCLI-D-13-00513.1
Page(s):
9727–9728
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Corresponding author address: Andréa S. Taschetto, University of New South Wales, Climate Change Research Centre and ARC Centre of Excellence for Climate System Science, Sydney NSW 2052, Australia. E-mail: a.taschetto@unsw.edu.au

Corresponding author address: Andréa S. Taschetto, University of New South Wales, Climate Change Research Centre and ARC Centre of Excellence for Climate System Science, Sydney NSW 2052, Australia. E-mail: a.taschetto@unsw.edu.au
Keywords: Australia; Indian Ocean; Atmosphere-ocean interaction; ENSO; Climate variability; Interannual variability

In Taschetto et al. (2011), Fig. 7b was mistakenly repeated in Fig. 7c. The correct figure for the IO+PO experiment appears as follows (i.e., with the corrected Fig. 7c). Note that this error does not affect the discussion or conclusions about the relative role of the Indian and Pacific Oceans with regard to Australian rainfall. Thus, no modification of the text is otherwise required.

Fig. 7.
Fig. 7.

Simulated JFM anomalies of sea level pressure (hPa) and winds (m s−1) at 850 hPa regressed onto the IOBW index: (a) IO, (b) PO, and (c) IO+PO experiments. Colored areas represent a response significant at the 95% confidence level according to a two-sided t test.

Citation: Journal of Climate 26, 23; 10.1175/JCLI-D-13-00513.1

REFERENCE

Taschetto, A. S., A. Sen Gupta, H. H. Hendon, C. C. Ummenhofer, and M. H. England, 2011: The contribution of Indian Ocean sea surface temperature anomalies on Australian summer rainfall during El Niño events. J. Climate, 24, 3734–3747.

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  • Taschetto, A. S., A. Sen Gupta, H. H. Hendon, C. C. Ummenhofer, and M. H. England, 2011: The contribution of Indian Ocean sea surface temperature anomalies on Australian summer rainfall during El Niño events. J. Climate, 24, 3734–3747.

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  • <sc>Fig</sc>. 7.
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    Fig. 7.

    Simulated JFM anomalies of sea level pressure (hPa) and winds (m s−1) at 850 hPa regressed onto the IOBW index: (a) IO, (b) PO, and (c) IO+PO experiments. Colored areas represent a response significant at the 95% confidence level according to a two-sided t test.

Fig. 7.

Simulated JFM anomalies of sea level pressure (hPa) and winds (m s−1) at 850 hPa regressed onto the IOBW index: (a) IO, (b) PO, and (c) IO+PO experiments. Colored areas represent a response significant at the 95% confidence level according to a two-sided t test.
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