Fig. 6: Spatial evolution of ISO rainfall in future projections and the difference between future and historical. | npj Climate and Atmospheric Science

Fig. 6: Spatial evolution of ISO rainfall in future projections and the difference between future and historical.

From: Equatorial convection controls boreal summer intraseasonal oscillations in the present and future climates

Fig. 6

Propagation composite of AAPM-SSP370 projections for the time 2080–2099 (a), and the difference between AAPM-SSP370 and AAPM-Historical (b). Shading represents the ISO-filtered rainfall anomalies (mm/day) and vectors ISO-filtered winds at 850 hpa level (m/s). Only those values which are significant at 95% (using a two-tailed t-test) are shaded in (a)). The days relative to day 0 are printed in the bottom right of each plot, and reference vectors are printed on the top right of each panel. Note the difference in the reference vector between the left and right panels. Refer to Supplementary Fig. 15 for the scaled version of (b).

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