Corrigendum

Hylke de Vries Department of Meteorology, University of Reading, Reading, United Kingdom

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Abstract

In a recent paper, explicit expressions have been derived for obtaining and subsequently partitioning streamfunction growth rates for a class of quasigeostrophic models. Unfortunately, however, some typographical errors have been made in the final representation of the equations. It is the aim of this corrigendum to give the correct expressions. The author notes that the results in the two-paper miniseries on “Resonance in Optimal Perturbation Evolution” by de Vries and Opsteegh have been obtained using the correct expressions, as listed as Eqs. (1),(3) below.

Corresponding author address: Dr. H. de Vries, Department of Meteorology, University of Reading, P.O. Box 243, Earley Gate, Reading RG6 6BB, United Kingdom. Email: h.devries@reading.ac.uk

Abstract

In a recent paper, explicit expressions have been derived for obtaining and subsequently partitioning streamfunction growth rates for a class of quasigeostrophic models. Unfortunately, however, some typographical errors have been made in the final representation of the equations. It is the aim of this corrigendum to give the correct expressions. The author notes that the results in the two-paper miniseries on “Resonance in Optimal Perturbation Evolution” by de Vries and Opsteegh have been obtained using the correct expressions, as listed as Eqs. (1),(3) below.

Corresponding author address: Dr. H. de Vries, Department of Meteorology, University of Reading, P.O. Box 243, Earley Gate, Reading RG6 6BB, United Kingdom. Email: h.devries@reading.ac.uk

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  • de Vries, H., and J. D. Opsteegh, 2007a: Resonance in optimal perturbation evolution. Part I: Two-layer Eady model. J. Atmos. Sci., 64 , 673694.

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  • de Vries, H., and J. D. Opsteegh, 2007b: Resonance in optimal perturbation evolution. Part II: Effects of a nonzero mean PV gradient. J. Atmos. Sci., 64 , 695710.

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