• LaCasce, J., 2012: Surface quasigeostrophic solutions and baroclinic modes with exponential stratification. J. Phys. Oceanogr., 42, 569580.

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  • 1 Department of Geosciences, University of Oslo, Oslo, Norway
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Corrigendum: Effect on spectra

Section 4e in the paper LaCasce (2012) compares the kinetic energy and buoyancy spectra obtained with constant and exponential stratification. The section was added during the revision of the first draft and added, evidently, too quickly. Figure 8 in LaCasce (2012) is half-way incorrect, and this affects the conclusions of the section.

The spectrum of the surface density is given in Eq. (27) in LaCasce (2012):where χ(z) is the vertical structure of the surface quasigeostrophic (SQG) solution, which depends on the stratification. The boundary condition

Corrigendum: Effect on spectra

Section 4e in the paper LaCasce (2012) compares the kinetic energy and buoyancy spectra obtained with constant and exponential stratification. The section was added during the revision of the first draft and added, evidently, too quickly. Figure 8 in LaCasce (2012) is half-way incorrect, and this affects the conclusions of the section.

The spectrum of the surface density is given in Eq. (27) in LaCasce (2012):where χ(z) is the vertical structure of the surface quasigeostrophic (SQG) solution, which depends on the stratification. The boundary condition

Corresponding author address: Joe LaCasce, University of Oslo, Department of Geosciences, P.O. Box 1022 Blindern, N-0315 Oslo, Norway. E-mail: j.h.lacasce@geo.uio.no
Corrigendum: Effect on spectra

Section 4e in the paper LaCasce (2012) compares the kinetic energy and buoyancy spectra obtained with constant and exponential stratification. The section was added during the revision of the first draft and added, evidently, too quickly. Figure 8 in LaCasce (2012) is half-way incorrect, and this affects the conclusions of the section.

The spectrum of the surface density is given in Eq. (27) in LaCasce (2012):where χ(z) is the vertical structure of the surface quasigeostrophic (SQG) solution, which depends on the stratification. The boundary condition

Corrigendum: Effect on spectra

Section 4e in the paper LaCasce (2012) compares the kinetic energy and buoyancy spectra obtained with constant and exponential stratification. The section was added during the revision of the first draft and added, evidently, too quickly. Figure 8 in LaCasce (2012) is half-way incorrect, and this affects the conclusions of the section.

The spectrum of the surface density is given in Eq. (27) in LaCasce (2012):where χ(z) is the vertical structure of the surface quasigeostrophic (SQG) solution, which depends on the stratification. The boundary condition

Corresponding author address: Joe LaCasce, University of Oslo, Department of Geosciences, P.O. Box 1022 Blindern, N-0315 Oslo, Norway. E-mail: j.h.lacasce@geo.uio.no
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