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Gregory S. Duane aInstitute for Mathematics and Its Applications, University of Minnesota, Minneapolis, Minnesota

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Joseph J. Tribbia bNational Center for Atmospheric Research, Boulder, Colorado

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© 2022 American Meteorological Society. For information regarding reuse of this content and general copyright information, consult the AMS Copyright Policy (www.ametsoc.org/PUBSReuseLicenses).

Corresponding author: Gregory S. Duane, gregory.duane@colorado.edu

© 2022 American Meteorological Society. For information regarding reuse of this content and general copyright information, consult the AMS Copyright Policy (www.ametsoc.org/PUBSReuseLicenses).

Corresponding author: Gregory S. Duane, gregory.duane@colorado.edu

In the published version of Duane and Tribbia (2004), Fig. 17 was a duplicate of Fig. 15. The correct version appears below. (The caption is unchanged from the published version.)

Fig. 17.
Fig. 17.

The forcing streamfunction ψ^* and blocking regions (boxes) for the two-sector model, as in Fig. 4, but with jets in latitudinally skewed positions.

Citation: Journal of the Atmospheric Sciences 79, 10; 10.1175/JAS-D-22-0143.1

REFERENCE

Duane, G. S., and J. J. Tribbia, 2004: Weak Atlantic–Pacific teleconnections as synchronized chaos. J. Atmos. Sci., 61, 21492168, https://doi.org/10.1175/1520-0469(2004)061<2149:WATASC>2.0.CO;2.

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  • Fig. 17.

    The forcing streamfunction ψ^* and blocking regions (boxes) for the two-sector model, as in Fig. 4, but with jets in latitudinally skewed positions.

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