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Corrigendum

Corrigendum 15 DECEMBER 2022 CO RR IG END U M 4659 a a DONG WAN KIM AND SUKYOUNG LEE Department of Meteorology and Atmospheric Science, The Pennsylvania State University, University Park, Pennsylvania (Manuscript received and in final form 23 November 2021) There was a computational error regarding the wave activity flux vectors shown in Figs. 2a–c of Kim and Lee (2021). We present the corrected Fig. 2 below. This change does not impact the major conclusion that the North Pacific Ocean and eastern Canada are the two main forcing regions. In fact, the corrected figure is more supportive of this conclusion because the wave activity flux vectors diverge from these two locations and the vectors are more parallel to the direction in which the destructive interference pattern propagates. We have also fixed a spelling error in the title of the figure. REFERENCE Kim, D. W., and S. Lee, 2021: Relationship between boreal summer circulation trend and destructive stationary–transient wave interference in the Western Hemisphere. J. Climate, 34, 4989–4999, https:// doi.org/10.1175/JCLI-D-20-0530.1. Corresponding author: Dong Wan Kim, dxk582@psu.edu DOI: 10.1175/JCLI-D-21-0913.1 For information regarding reuse of this content and general copyright information, consult the AMS Copyright Policy (www.ametsoc.org/ PUBSReuseLicenses). 4660 JOURNAL OF CLIMATE http://www.deepdyve.com/assets/images/DeepDyve-Logo-lg.png Journal of Climate American Meteorological Society

Corrigendum

Kim, Dong Wan; Lee, Sukyoung
Journal of Climate , Volume 35 (24): 2 – Dec 15, 2022
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Publisher
American Meteorological Society
Copyright
Copyright © American Meteorological Society
ISSN
1520-0442
eISSN
1520-0442
DOI
10.1175/jcli-d-21-0913.1
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Abstract

15 DECEMBER 2022 CO RR IG END U M 4659 a a DONG WAN KIM AND SUKYOUNG LEE Department of Meteorology and Atmospheric Science, The Pennsylvania State University, University Park, Pennsylvania (Manuscript received and in final form 23 November 2021) There was a computational error regarding the wave activity flux vectors shown in Figs. 2a–c of Kim and Lee (2021). We present the corrected Fig. 2 below. This change does not impact the major conclusion that the North Pacific Ocean and eastern Canada are the two main forcing regions. In fact, the corrected figure is more supportive of this conclusion because the wave activity flux vectors diverge from these two locations and the vectors are more parallel to the direction in which the destructive interference pattern propagates. We have also fixed a spelling error in the title of the figure. REFERENCE Kim, D. W., and S. Lee, 2021: Relationship between boreal summer circulation trend and destructive stationary–transient wave interference in the Western Hemisphere. J. Climate, 34, 4989–4999, https:// doi.org/10.1175/JCLI-D-20-0530.1. Corresponding author: Dong Wan Kim, dxk582@psu.edu DOI: 10.1175/JCLI-D-21-0913.1 For information regarding reuse of this content and general copyright information, consult the AMS Copyright Policy (www.ametsoc.org/ PUBSReuseLicenses). 4660 JOURNAL OF CLIMATE

Journal

Journal of Climate – American Meteorological Society

Published: Dec 15, 2022

References

  • Relationship between boreal summer circulation trend and destructive stationary–transient wave interference in the Western Hemisphere
    Kim, D. W.; Lee, S.