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

• Published in: Quarterly journal of the Royal Meteorological Society Vol. 145; no. 723; pp. 2586 - 2602
• Main Authors: Imran, Hosen M., Kala, Jatin, Ng, Anne W. M., Muthukumaran, Shobha
• Format: Journal Article
• Language: English
• Published: Chichester, UK John Wiley & Sons, Ltd 01-07-2019; Wiley Subscription Services, Inc
• Subjects: coupled WRF–SLUCM model; Duration; Expansion; Heat; Heat flux; Heat transfer; Heat waves; Heatwaves; human thermal comfort; Meteorology; Plant cover; Rural areas; Skin; Storage; Surface temperature; Thermal comfort; Urban areas; urban expansion; urban heat island; Urban heat islands; Urban meteorology; Urban sprawl; Weather forecasting; Australia
• ISSN: 0035-9009; 1477-870X
• DOI: 10.1002/qj.3580

The city of Melbourne in southeast Australia is planning to expand urban areas substantially by the year 2050 and this expansion has the potential to alter the Urban Heat Island (UHI), that is, higher temperatures in urban areas as compared to surrounding rural areas. Moreover, Melbourne has been experiencing more frequent heatwaves for last two decades, and the intensity and duration of heatwaves is expected to increase in the future, which could exacerbate the UHI. This study evaluates the potential impacts of future urban expansion on the urban meteorology in Melbourne city during four of the most severe heatwave events during the period 2000–2009. Urban expansion is implemented as high‐density urban with a high urban fraction of 0.9 to investigate the maximum possible impact. Simulations are carried out using the Weather Research and Forecasting model coupled with the Single‐Layer Urban Canopy Model with current land‐use and future urban expansion scenarios. Urban expansion increases the near‐surface (2‐m) UHI (UHI2) by 0.75 to 2.80 °C and the skin‐surface UHI (UHIsk) by 1.9 to 5.4 °C over the expanded urban areas during the night, with no changes in existing urban areas. No substantial changes in UHI2 and UHIsk occur during the day over both existing and expanded urban areas. This is largely driven by changes in the storage heat flux, with an increase in storage heat at night and a decrease during the day; that is, excess storage heat accumulated during the day is released at night, which causes a slower decrease of near‐surface temperature and increase in the UHI. Urban expansion did not affect human thermal comfort (HTC) in existing urban areas and there were no marked differences in HTC between existing and expanded urban areas.
(a) Model nested domain configuration (the boundary represents the outer domain with a resolution of 18 km, and d02 and d03 denote the boundaries of the two inner nested domains, with resolutions of 6 and 2 km respectively), (b) current distribution of urban land use, (c) high‐density urban expansion according to Plan Melbourne 2050. The numbers 31, 32, and 33 represent the low‐density urban, high‐density urban, and commercial/industrial areas, respectively.