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. 2017 May 8;372(1723):20160147. doi: 10.1098/rstb.2016.0147

Figure 1.

Figure 1.

The distribution (and 99% quantiles: dashed vertical lines) of maximum daily temperature (°C) broadens and shifts toward lower temperatures as the latitudes of weather stations increase along latitudinal gradients (at 5° intervals) in the centres of (a) North America (−100 °E) and (b) Asia (77.5 °E).