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Journal of Physical Oceanography

  • Blaker, A. T., J. J.-M. Hirschi, B. Sinha, B. de Cuevas, S. Alderson, A. Coward, and G. Madec, 2012: Large near-inertial oscillations of the Atlantic meridional overturning circulation. Ocean Modell., 42, 50–56.

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  • Sévellec, F., J. J.-M. Hirschi, and A. T. Blaker, 2013: On the near-inertial resonance of the Atlantic meriodional overturning circulation. J. Phys. Oceanogr., 43, 2661–2672, doi:10.1175/JPO-D-13-092.1.

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Editorial Type:
Corrigendum
Article Type:
Correction

CORRIGENDUM

Florian Sévellec1, Joël J.-M. Hirschi2, and Adam T. Blaker2
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  • 1 Ocean and Earth Science, National Oceanography Centre Southampton, University of Southhapton, Southampton, United Kingdom
  • | 2 National Oceanography Centre, Southampton, Southampton, United Kingdom
Print Publication:
01 Nov 2014
DOI:
https://doi.org/10.1175/JPO-D-14-0180.1
Page(s):
2987–2988
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Two production errors occurred in Sévellec et al. (2013). In both Figs. 5 and 6, titles above the figures panels were incorrectly removed, leaving the two figures without units (hour and m s−1, respectively). Those figures appear below as they were meant to appear originally.

Period (hour) of the max amplitude response of the vertical shear for the geo- (black lines) and ageostrophic (gray lines) terms following (11) and (16), respectively. Solid lines represent the result for ε = 2 × 10−5 s−1,

Two production errors occurred in Sévellec et al. (2013). In both Figs. 5 and 6, titles above the figures panels were incorrectly removed, leaving the two figures without units (hour and m s−1, respectively). Those figures appear below as they were meant to appear originally.

Period (hour) of the max amplitude response of the vertical shear for the geo- (black lines) and ageostrophic (gray lines) terms following (11) and (16), respectively. Solid lines represent the result for ε = 2 × 10−5 s−1,

Corresponding author address: Florian Sévellec, Ocean and Earth Science, University of Southampton, Waterfront Campus, European Way, Southampton, SO14 3ZH, United Kingdom. E-mail: florian.sevellec@noc.soton.ac.uk

Two production errors occurred in Sévellec et al. (2013). In both Figs. 5 and 6, titles above the figures panels were incorrectly removed, leaving the two figures without units (hour and m s−1, respectively). Those figures appear below as they were meant to appear originally.

Period (hour) of the max amplitude response of the vertical shear for the geo- (black lines) and ageostrophic (gray lines) terms following (11) and (16), respectively. Solid lines represent the result for ε = 2 × 10−5 s−1,

Two production errors occurred in Sévellec et al. (2013). In both Figs. 5 and 6, titles above the figures panels were incorrectly removed, leaving the two figures without units (hour and m s−1, respectively). Those figures appear below as they were meant to appear originally.

Period (hour) of the max amplitude response of the vertical shear for the geo- (black lines) and ageostrophic (gray lines) terms following (11) and (16), respectively. Solid lines represent the result for ε = 2 × 10−5 s−1,

Corresponding author address: Florian Sévellec, Ocean and Earth Science, University of Southampton, Waterfront Campus, European Way, Southampton, SO14 3ZH, United Kingdom. E-mail: florian.sevellec@noc.soton.ac.uk
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