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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 and 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.
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 ...
However, the monsoon is not a simple response to heating but a more complex interaction of topography, wind and sea, as demonstrated by its abrupt rather than gradual withdrawal from the region. The Australian monsoon (the "Wet") occurs in the southern summer when the monsoon trough develops over Northern Australia. Over three-quarters of ...
The monsoon climate of northern Australia is hot and humid in summer. ... (104 °F) in the inland Pilbara and Kimberley before the wet season breaks. Further north ...
There is less risk of frost, [13] but increased risk of widespread flooding, tropical cyclones, and the monsoon season starts earlier. [14] La Niña Modoki leads to a rainfall increase over northwestern Australia and northern Murray–Darling basin, rather than over the east as in a conventional La Niña. [15]
The rainfall distribution by month in Cairns, Australia. The wet season (sometimes called the rainy season or monsoon season) is the time of year when most of a region's average annual rainfall occurs. [1] Generally, the season lasts at least one month. [2] The term green season is also sometimes used as a euphemism by tourist authorities. [3]
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.
Monsoon forests grow in tropical areas of northern Australia with a pronounced dry season. They are typically semi-deciduous, with many canopy trees losing their leaves during the dry season, and becoming 'raingreen' during the rainy monsoon season.