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Nicole Feldl Department of Atmospheric Sciences, University of Washington, Seattle, Washington

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Gerard H. Roe Department of Earth and Space Sciences, University of Washington, Seattle, Washington

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Corresponding author address: Nicole Feldl, Department of Atmospheric Sciences, University of Washington, Box 351640, Seattle, WA 98195-1640. E-mail: feldl@uw.edu

Corresponding author address: Nicole Feldl, Department of Atmospheric Sciences, University of Washington, Box 351640, Seattle, WA 98195-1640. E-mail: feldl@uw.edu

Because of an oversight, the caption for Fig. 8 in Feldl and Roe (2013) contains an error. The correct figure and caption appear below as they should have appeared.

Fig. 8.
Fig. 8.

(a) Zonal-mean change in fractional specific humidity, relative to a 1-K warming and fixed relative humidity, averaged over 9 months (filled contours). Contour lines show streamlines for control climate. (b) Two estimates of the nonlinear term (W m−2). Nonlinearity is due to interactions among and within clear-sky feedbacks (solid) for the same time period as (a). Plotted for comparison is the residual nonlinearity (dashed) of Fig. 5.

Citation: Journal of Climate 27, 5; 10.1175/JCLI-D-14-00031.1

We regret any inconvenience this error may have caused.

REFERENCE

Feldl, N., and G. H. Roe, 2013: The nonlinear and nonlocal nature of climate feedbacks. J. Climate, 26, 82898304.

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  • Feldl, N., and G. H. Roe, 2013: The nonlinear and nonlocal nature of climate feedbacks. J. Climate, 26, 82898304.

  • Fig. 8.

    (a) Zonal-mean change in fractional specific humidity, relative to a 1-K warming and fixed relative humidity, averaged over 9 months (filled contours). Contour lines show streamlines for control climate. (b) Two estimates of the nonlinear term (W m−2). Nonlinearity is due to interactions among and within clear-sky feedbacks (solid) for the same time period as (a). Plotted for comparison is the residual nonlinearity (dashed) of Fig. 5.

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