CORRIGENDUM

Florian Sévellec Ocean and Earth Science, National Oceanography Centre Southampton, University of Southhapton, Southampton, United Kingdom

Search for other papers by Florian Sévellec in
Current site
Google Scholar
PubMed
Close
,
Joël J.-M. Hirschi National Oceanography Centre, Southampton, Southampton, United Kingdom

Search for other papers by Joël J.-M. Hirschi in
Current site
Google Scholar
PubMed
Close
, and
Adam T. Blaker National Oceanography Centre, Southampton, Southampton, United Kingdom

Search for other papers by Adam T. Blaker in
Current site
Google Scholar
PubMed
Close
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
  • 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
  • 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).

  • 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).

All Time Past Year Past 30 Days
Abstract Views 0 0 0
Full Text Views 175 73 1
PDF Downloads 48 20 5