Figures and Tables

From the following article:

Weakening of tropical Pacific atmospheric circulation due to anthropogenic forcing

Gabriel A. Vecchi, Brian J. Soden, Andrew T. Wittenberg, Isaac M. Held, Ants Leetmaa & Matthew J. Harrison

Nature 441, 73-76(4 May 2006)

doi:10.1038/nature04744

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Figure 1 - Unfortunately we are unable to provide accessible alternative text for this. If you require assistance to access this image, or to obtain a text description, please contact npg@nature.com

Figure 1

Spatial pattern of observed and modelled sea level pressure linear trends.

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Figure 2

Summary of the linear trends in SLP gradient across the Indo-Pacific (DeltaSLP) from observations and the various GCM historical radiative forcing experiments.

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Figure 3

Observed and modelled evolution of DeltaSLP since the nineteenth century.

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Figure 4

Observed and modelled equatorial Pacific zonal-mean zonal wind-stress anomaly, <taux > , and equatorial thermocline depth anomaly, Ztc.

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