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Impacts of future urban expansion on urban heat island effects during heatwave events in the city of Melbourne in southeast Australia

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Figure 2 shows the mean daily mean sea-level pressure(MSLP), wind speed with direction at 10 m, and poten-tial temperature at 850 hPa from the outermost domain(Figure 1a)
Figure 4, but are discussed in more detail in later in the arti-cle in Figure 10, as changes are of opposite sign during theday and night and hence are shown separately)
Figure 12 (top) shows the hourly variation in the UTCI for thefour control experiments, in which the strongest human ther-mal stress occurs between midday and afternoon, and the most

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