Editorial Type:
Corrigendum
Article Type:
Correction

CORRIGENDUM

David J. Stephens Department of Agriculture and Food WA, South Perth, Western Australia, Australia

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,
Harry van Loon Colorado Research Associates/Northwest Research Associates, Boulder, Colorado

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Malcolm H. Lamond Lamond Weather Services, Karrinyup, Western Australia, Australia

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Nicola P. Telcik Yarra Valley Water, Mitcham, Victoria, Australia

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Print Publication:
15 May 2008
DOI:
https://doi.org/10.1175/JCLI2502.1
Page(s):
2332–2333
Full access

Due to an error, an incorrect version of Fig. 8 in Stephens et al. (2007) was published in which the x-axis labels were not accurately placed. The correct version of Fig. 8 is presented below.

REFERENCES

Stephens, D. J., M. J. Meuleners, H. van Loon, M. H. Lamond, and N. P. Telcik, 2007: Differences in atmospheric circulation between the development of weak and strong warm events in the Southern Oscillation. J. Climate, 20 , 2191–2209.

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Fig. 8.
Fig. 8.

(a) Plot of normalized Rapa Island SLP anomalies since 1951 (black line, left y axis) vs actual Niño-3 SST anomalies (red and blue shading, right y axis). (b) Plot of normalized Niño-3 SST anomalies (red curve) vs normalized Rapa Island SLP anomalies (blue curve) and normalized 850-hPa west Pacific trade winds (purple curve), 1979–2004. All curves have been smoothed using a 5-month running mean.

Citation: Journal of Climate 21, 10; 10.1175/JCLI2502.1

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Journal of Climate

  • Stephens, D. J., M. J. Meuleners, H. van Loon, M. H. Lamond, and N. P. Telcik, 2007: Differences in atmospheric circulation between the development of weak and strong warm events in the Southern Oscillation. J. Climate, 20 , 2191–2209.

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  • <sc>Fig</sc>. 8.
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    Fig. 8.

    (a) Plot of normalized Rapa Island SLP anomalies since 1951 (black line, left y axis) vs actual Niño-3 SST anomalies (red and blue shading, right y axis). (b) Plot of normalized Niño-3 SST anomalies (red curve) vs normalized Rapa Island SLP anomalies (blue curve) and normalized 850-hPa west Pacific trade winds (purple curve), 1979–2004. All curves have been smoothed using a 5-month running mean.

Fig. 8.

(a) Plot of normalized Rapa Island SLP anomalies since 1951 (black line, left y axis) vs actual Niño-3 SST anomalies (red and blue shading, right y axis). (b) Plot of normalized Niño-3 SST anomalies (red curve) vs normalized Rapa Island SLP anomalies (blue curve) and normalized 850-hPa west Pacific trade winds (purple curve), 1979–2004. All curves have been smoothed using a 5-month running mean.
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