Corrigendum: The non-Gaussianity and spatial asymmetry of temperature extremes relative to the storm track: The role of horizontal advection [J. Climate, 30, (2017) (445-464)] DOI:10.1175/JCLI-D-15-0806.1

Chaim I. Garfinkel; Darryn W. Waugh

doi:10.1175/JCLI-D-18-0850.1

Corrigendum: The non-Gaussianity and spatial asymmetry of temperature extremes relative to the storm track: The role of horizontal advection [J. Climate, 30, (2017) (445-464)] DOI:10.1175/JCLI-D-15-0806.1

Chaim I. Garfinkel^*, Darryn W. Waugh

^*Corresponding author for this work

Fredy & Nadine Herrmann Institute of Earth Sciences

Research output: Contribution to journal › Comment/debate

Abstract

Atypo was included in Eq. (2) of Garfinkel et al. (2013), Garfinkel and Waugh (2014), and Garfinkel and Harnik (2017). The equation should read as follows: All modeling experiments in Garfinkel et al. (2013), Garfinkel and Waugh (2014), and Garfinkel and Harnik (2017) were forced with δT_new as formulated here, and hence this error did not affect the results or conclusions of any of the three original papers. Note that the last term on the right-hand side of the equation leads to a temperature perturbation in the midlatitudes near 508, and not at 158 as was mistakenly written.

Original language	English
Pages (from-to)	2167
Number of pages	1
Journal	Journal of Climate
Volume	32
Issue number	7
DOIs	https://doi.org/10.1175/JCLI-D-18-0850.1
State	Published - 1 Apr 2019

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© 2019 American Meteorological Society.

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abstract = "Atypo was included in Eq. (2) of Garfinkel et al. (2013), Garfinkel and Waugh (2014), and Garfinkel and Harnik (2017). The equation should read as follows: All modeling experiments in Garfinkel et al. (2013), Garfinkel and Waugh (2014), and Garfinkel and Harnik (2017) were forced with δTnew as formulated here, and hence this error did not affect the results or conclusions of any of the three original papers. Note that the last term on the right-hand side of the equation leads to a temperature perturbation in the midlatitudes near 508, and not at 158 as was mistakenly written.",

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Corrigendum: The non-Gaussianity and spatial asymmetry of temperature extremes relative to the storm track: The role of horizontal advection [J. Climate, 30, (2017) (445-464)] DOI:10.1175/JCLI-D-15-0806.1

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