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A thunderstorm in Sydney. The climate of Sydney, Australia is humid subtropical (Köppen: Cfa), [1] shifting from mild [2] [3] [4] and cool [5] in winter to warm and occasionally hot [5] in the summer, with no extreme seasonal differences since the weather has some maritime influence (as it is moderated by proximity to the Pacific Ocean). [3]
On 26 July 1952, Sydney CBD received 203.2 mm (8.00 in) of rain and cyclonic winds caused local floods, two landslides in the north, traffic delays and as well as a death of a man. [92] On 10 February 1956, heavy rain caused the Georges River to overflow, which led to five deaths, flooding 1,000 homes and leading to the evacuation of 8,000 people.
South Australia's mean temperature range is 29 °C (84 °F) in January and 15 °C (59 °F) in July. Daily temperatures in parts of the state in January and February can be up to 50 °C (122 °F). The highest maximum temperature was recorded as 50.7 °C (123.3 °F) at Oodnadatta on 2 January 1960, which is the highest official temperature ...
The July flood event was the fourth major flood to strike Western Sydney in less than two years, with the weekend (July 2–3) receiving as much rainfall as Melbourne, Canberra or London generally receive in a year. The heaviest amount had fallen in Brogers Creek, where 933 mm (36.73 in) of rain fell in four days. [21]
A southerly buster is the colloquial name [1] of an abrupt southerly wind change in the southern regions of New South Wales and Victoria, Australia, which approaches from the southeast, mainly on a hot day, bringing in cool, usually severe weather and a dramatic temperature drop, thus ultimately replacing and relieving the prior hot conditions.
In Sydney, 'snow' was last alleged on 28 June 1836, where British settlers in Hyde Park claimed to have woken up to "snow nearly 1 in (2.5 cm) deep" – However, after a fall of graupel in July 2008, the Bureau of Meteorology had doubted the 1836 'snow' account, stating that observers in that era lacked the technology to distinguish snow from ...
Wet season storm in Darwin. In northern Australia, the predominant wind is from the east or southeast in most occasions, which usually bring dry conditions. [4] Though during monsoon periods (between November to April), the winds change to northwesterly, where atmospheric pressure decreases over an area extending to Java, Sumatra, Timor Sea and eastward to Papua New Guinea.
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