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The region of Sydney is subject to phenomena typical of a microclimate, namely in late spring and summer, where the western suburbs are hotter than the Sydney CBD by 6–10 °C (11–18 °F) [73] due to urban sprawl exacerbating the urban heat island effect and less exposure to mitigating sea breezes which cool down Sydney's eastern edge and ...
Autumn lasts between March and May and experiences changeable weather, where summer weather patterns gradually take on the shape of winter patterns. [48] The highest recorded maximum temperature in Tasmania was 42.2 °C (108.0 °F) at Scamander on 30 January 2009, during the 2009 south-eastern Australia heat wave. Tasmania's lowest recorded ...
On 27 November 2024, after a nearly a week-long heatwave conditions in Sydney, where the City saw weather conditions more typical of January or February than in November. Sydney Airport warmed to 38.1 °C (100.6 °F) at 12:15pm, which made it the hottest place in the world at that time (a few reasons being due to the foehn effect and UHI effect).
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In September, when the foehn effect is usually strong, green pastures on the windward side (left, Central Tablelands) can be contrasted from the dry landscape on the leeward (right, Greater Western Sydney). 28 May 2000 was a striking example of the 'divided' weather between the western and eastern faces of the range.
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Unlike the rest of the state, this region receives the majority of its snow events from southerly weather systems (being largely sheltered from the west). In southern Victoria and West Gippsland , there is a greater chance of late spring and summer snowfall, with an occurrence of snow on 25 December 2006 in the Dandenong Ranges , not more than ...
An east coast low on 27 July 2020 taken by Himawari 8. Australian east coast lows (known locally as east coast lows, maritime lows, and east coast cyclones [1]) are extratropical cyclones or low-pressure systems on the coast of southeastern Australia that may be caused by both mid-latitude and tropical influences over a variety of levels in the atmosphere.