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The Australian monsoon (AUM), also known as the Australian summer monsoon (ASM), [2] and the Australian-Indonesian monsoon (AIM), [3] is a monsoon system that increases thunderstorms and rainfall over many areas of Indonesia and northern Australia, from the far northern tropics of the region to the semi-arid zone of Australia, typically between ...
A billabong in the Kakadu National Park, Northern Territory. The monsoon climate of northern Australia is hot and humid in summer. The tropical savannah zone of Northern Australia is warm to hot all year. Summers are hot in most of the country with average January maximum temperatures exceeding 30 °C over most of the mainland, except for high ...
The conditions were described as unusual for the season, particularly in the Northern Territory, where monsoonal weather would typically be expected during this time. [2] He predicted that the temperatures would be the hottest observed in Australia since the " Black Summer " heatwaves in 2019–2020. [ 3 ]
The onset of the monsoon over Australia tends to follow the heating maxima down Vietnam and the Malay Peninsula (September), to Sumatra, Borneo and the Philippines (October), to Java, Sulawesi (November), Irian Jaya and northern Australia (December, January). However, the monsoon is not a simple response to heating but a more complex ...
Monthly average maximum temperatures range from 25 to 35 °C (77 to 95 °F). The monsoon brings a summer wet season between November and March. The dry season extends for the rest of the year, and is nearly rainless. Rainfall generally decreases from north to south, ranging from 1200 mm per year in the north to 600 mm per year in the south.
During February 2024, the presence of the Madden–Julian Oscillation and an equatorial Indian Ocean in the Australian region contributed to the formation of Tropical Low 07U in the monsoon trough over the western Gulf of Carpentaria, [89] [90] [91] approximately 419 km (260 mi) to the east-southeast of Darwin in the Northern Territory during ...
August position of the ITCZ and monsoon trough in the Pacific Ocean, depicted by area of convergent streamlines in the northern Pacific. The monsoon trough is a portion of the Intertropical Convergence Zone in the Western Pacific, [1] [2] as depicted by a line on a weather map showing the locations of minimum sea level pressure, [1] and as such, is a convergence zone between the wind patterns ...
Within the basin, most tropical cyclones have their origins within the South Pacific convergence zone or within the Northern Australian monsoon trough, both of which form an extensive area of cloudiness and are dominant features of the season. Within this region a tropical disturbance is classified as a tropical cyclone when it has 10-minute ...