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CORRIGENDUM

CORRIGENDUM The rotation angle of the principal axis for two locations in Schaeffer et al. (2013) was incorrectly reported. The major axis orientation in Table 1 for both CH070 and CH100 should read 20° and not 7°. This resulted in an error in Fig. 1b of Schaeffer et al. (2013) . The correct Table 1 and Fig. 1 appear below. This does not affect any of the analysis or conclusions. The authors regret any inconvenience this error may have caused. Table 1. Mooring information. The temporal coverage is calculated over a period of 2 yr, from January 2010 to December 2011. Fig . 1. (a) Sea surface temperature (3-day composite) and geostrophic currents on 7 Jan 2010. Mean depth-averaged current vectors and variance ellipses at (b) Coffs Harbour (CH070 and CH100) and (c) Sydney (ORS065, SYD100, and SYD140) moorings. The mean wind stress from the meteorological stations is shown in gray. The coastline and 20-, 100-, 200-, 500-, 1000-, and 2000-m isobaths are shown, with bold lines for 200 and 2000 m. http://www.deepdyve.com/assets/images/DeepDyve-Logo-lg.png Journal of Physical Oceanography American Meteorological Society

CORRIGENDUM

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References (1)

Publisher
American Meteorological Society
Copyright
Copyright © 2014 American Meteorological Society
ISSN
0022-3670
eISSN
1520-0485
DOI
10.1175/JPO-D-14-0091.1
Publisher site
See Article on Publisher Site

Abstract

The rotation angle of the principal axis for two locations in Schaeffer et al. (2013) was incorrectly reported. The major axis orientation in Table 1 for both CH070 and CH100 should read 20° and not 7°. This resulted in an error in Fig. 1b of Schaeffer et al. (2013) . The correct Table 1 and Fig. 1 appear below. This does not affect any of the analysis or conclusions. The authors regret any inconvenience this error may have caused. Table 1. Mooring information. The temporal coverage is calculated over a period of 2 yr, from January 2010 to December 2011. Fig . 1. (a) Sea surface temperature (3-day composite) and geostrophic currents on 7 Jan 2010. Mean depth-averaged current vectors and variance ellipses at (b) Coffs Harbour (CH070 and CH100) and (c) Sydney (ORS065, SYD100, and SYD140) moorings. The mean wind stress from the meteorological stations is shown in gray. The coastline and 20-, 100-, 200-, 500-, 1000-, and 2000-m isobaths are shown, with bold lines for 200 and 2000 m.

Journal

Journal of Physical Oceanography – American Meteorological Society

Published: Apr 16, 2014

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