• Luo, D., Y. Yao, A. Dai, and S. Feldstein, 2015: The positive North Atlantic Oscillation with downstream blocking and Middle East snowstorms: The large-scale environment. J. Climate, 28, 63986418, doi:10.1175/JCLI-D-15-0184.1.

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    Composite vertically integrated moisture flux vectors at lag 0 for six classifications of EB events: (a) northward-displaced EB-related NAO+ events, (b) dipole-type EB events, (c) strong EB events, (d) southward-displaced EB-related NAO+ events, (e) omega-type EB events, and (f) weak EB events. In each panel, the green (blue) region denotes precipitation (negative temperature anomaly). The reference vector magnitude arrows at the top right of each panel indicate the magnitude of the flux vector scaled by 1000 kg m−1 s−1.

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  • 1 RCE-TEA, Institute of Atmospheric Physics, Chinese Academy of Science, Beijing, China
  • | 2 Department of Atmospheric and Environmental Sciences, University at Albany, State University of New York, Albany, New York, and National Center for Atmospheric Research, Boulder, Colorado
  • | 3 Department of Meteorology, The Pennsylvania State University, University Park, Pennsylvania
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Corresponding author address: Dr. Dehai Luo, RCE-TEA, Institute of Atmospheric Physics, Chinese Academy of Science, Huayanli No. 40, Beijing 100029, China. E-mail: ldh@mail.iap.ac.cn

Corresponding author address: Dr. Dehai Luo, RCE-TEA, Institute of Atmospheric Physics, Chinese Academy of Science, Huayanli No. 40, Beijing 100029, China. E-mail: ldh@mail.iap.ac.cn

In Luo et al. (2015), the figure caption in Fig. 15 was mistakenly written. The corrected caption appears below.

Fig. 15.
Fig. 15.

Composite vertically integrated moisture flux vectors at lag 0 for six classifications of EB events: (a) northward-displaced EB-related NAO+ events, (b) dipole-type EB events, (c) strong EB events, (d) southward-displaced EB-related NAO+ events, (e) omega-type EB events, and (f) weak EB events. In each panel, the green (blue) region denotes precipitation (negative temperature anomaly). The reference vector magnitude arrows at the top right of each panel indicate the magnitude of the flux vector scaled by 1000 kg m−1 s−1.

Citation: Journal of Climate 29, 21; 10.1175/JCLI-D-16-0008.1

The authors regret any inconvenience these errors may have caused.

REFERENCE

Luo, D., Y. Yao, A. Dai, and S. Feldstein, 2015: The positive North Atlantic Oscillation with downstream blocking and Middle East snowstorms: The large-scale environment. J. Climate, 28, 63986418, doi:10.1175/JCLI-D-15-0184.1.

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