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Adelaide has a Mediterranean climate characterised by dry summers and wet winters, with approximately 550 mm of annual rainfall concentrated between June and August. While lower than east-coast capitals, this seasonal concentration means a significant volume of water falls in a short window — overwhelming stormwater infrastructure and saturating soils that have been dry for months.
The Torrens and Onkaparinga river catchments span large sections of the metro area, and catchment events during heavy winter storms can produce rapid inundation of low-lying suburbs. The Adelaide Hills face fast-moving runoff that channels into creek systems and reaches metro Adelaide within hours of a storm event.
Inner-suburb infrastructure presents a particular risk: ageing clay or cast-iron pipes in pre-1970s housing stock are highly susceptible to burst events. Adelaide's reactive clay soils expand significantly in winter and shrink in dry summers, placing cyclical stress on buried pipework that can lead to sudden failures without warning.
priority emergency response across Greater Adelaide:
Inner / CBD: Adelaide CBD, North Adelaide, Norwood, Unley, Mitcham, Glenelg, Parkside, Prospect, Kensington, Fullarton
Northern Suburbs: Elizabeth, Salisbury, Para Hills, Modbury, Tea Tree Gully, Golden Grove, Mawson Lakes, Pooraka
Southern Suburbs: Noarlunga, Morphett Vale, Reynella, Hallett Cove, Seaford, Christies Beach, Hackham, Woodcroft
Eastern Hills: Stirling, Aldgate, Bridgewater, Mount Barker, Crafers, Blackwood, Belair
Western / Port: Port Adelaide, Semaphore, Le Fevre Peninsula, Largs Bay, Exeter, Peterhead
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