Supplemental Fig. A – Table version of Fig. 6 provided with

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Supplemental Figures

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Supplemental Fig. A – Table version of Ошибка! Источник ссылки не найден.

provided with quantitative values. Values in each cell depict the average monthly value of centerline shift

(degrees of latitude) between each respective GCM and the averaged location from GPCP and

TRMM observations, given as the model minus the observations. Cells are shaded blue (red) in increasing intensity when the centerline of the GCM was found to be more northward

(southward) compared to the observations. The color of the text used within the cells is irrelevant within these supplemental figures and is only varied to provide easier reading and more contrast in available colors.

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Supplemental Fig. B – Table version of Ошибка! Источник ссылки не найден.

a provided with quantitative values. Values in each cell depict the difference in average monthly ITCZ width (degrees of latitude) between each respective GCM and GPCP observations, given as the model minus observations. Cells are shaded red (blue) in increasing intensity when the width of the ITCZ simulated by the GCM was found to be wider (thinner) compared to the GPCP ITCZ width.

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Supplemental Fig. C – Same as Fig. B but using TRMM observational results ( Ошибка!

Источник ссылки не найден.

b).

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Supplemental Fig. D – Table version of Figure 8a provided with quantitative values. Values in each cell depict the difference in precipitation (mm/day) between each GCM simulation and

GPCP observation when averaged within ±4° latitude of the observed centerline, given as the model minus observations. Cells are shaded red (blue) in increasing intensity when the magnitude of precipitation in the GCM was found to be stronger (weaker) compared to the magnitude of precipitation within the GPCP ITCZ.

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Supplemental Fig. E – Same as Fig. D but using TRMM observational results (Fig. 8b).

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Supplemental Fig. F - Table version of Ошибка! Источник ссылки не найден.

provided with quantitative values. Values in each cell depict the differences in precipitation (mm/day) between CMIP and AMIP simulations when averaged within ±4° latitude of the observed centerline, given as CMIP minus AMIP. Cells are shaded red (blue) in increasing intensity when the magnitude of precipitation in the CMIP version of the GCM was found to be stronger

(weaker) compared to its AMIP counterpart.

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