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, 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
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
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
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
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
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, 50–56.
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.
