• 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, 5056.

    • Search Google Scholar
    • Export Citation
  • 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, 26612672, doi:10.1175/JPO-D-13-092.1.

    • Search Google Scholar
    • Export Citation
  • View in gallery

    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, the gray lines in Figs. 3b and 4b, respectively. Dashed lines represent the result for ε = 5 × 10−5 s−1, the gray lines in Figs. 3c and 4c, respectively. The thin black line indicates the inertial period. The crosses denote the AMOC variability period from the ¼° OGCM experiments by Blaker et al. (2012).

  • View in gallery

    Phase and group velocities [cp (solid lines) and cg (dashed lines), respectively] of the Poincaré waves for a 5° wavelength as a function of latitude (m s−1). These results follow the analytical expression of (22), where a negative value of these curves is also a possible solution. The crosses denote the phase velocities from the ¼° OGCM experiments by Blaker et al. (2012).

All Time Past Year Past 30 Days
Abstract Views 0 0 0
Full Text Views 43 41 4
PDF Downloads 18 17 4

CORRIGENDUM

View More View Less
  • 1 Ocean and Earth Science, National Oceanography Centre Southampton, University of Southhapton, Southampton, United Kingdom
  • | 2 National Oceanography Centre, Southampton, Southampton, United Kingdom
© Get Permissions
Full access

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

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.

Fig. 5.
Fig. 5.

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, the gray lines in Figs. 3b and 4b, respectively. Dashed lines represent the result for ε = 5 × 10−5 s−1, the gray lines in Figs. 3c and 4c, respectively. The thin black line indicates the inertial period. The crosses denote the AMOC variability period from the ¼° OGCM experiments by Blaker et al. (2012).

Citation: Journal of Physical Oceanography 44, 11; 10.1175/JPO-D-14-0180.1

Fig. 6.
Fig. 6.

Phase and group velocities [cp (solid lines) and cg (dashed lines), respectively] of the Poincaré waves for a 5° wavelength as a function of latitude (m s−1). These results follow the analytical expression of (22), where a negative value of these curves is also a possible solution. The crosses denote the phase velocities from the ¼° OGCM experiments by Blaker et al. (2012).

Citation: Journal of Physical Oceanography 44, 11; 10.1175/JPO-D-14-0180.1

The staff of the Journal of Physical Oceanography regrets any inconvenience these errors may have caused.

REFERENCES

  • 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, 5056.

    • Search Google Scholar
    • Export Citation
  • 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, 26612672, doi:10.1175/JPO-D-13-092.1.

    • Search Google Scholar
    • Export Citation
Save