Search results
Results from the WOW.Com Content Network
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.
The monsoon climate of northern Australia is hot and humid in summer. ... location and date °C ... history occurred during the 2019–2020 Australian bushfire season
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.
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]
The monsoon climate of northern Australia is hot and humid in summer. ... the rainfall over the wet season can vary from less than 100 millimetres (3.9 in) ...
There are approximately 1500 monsoon rainforest patches totaling 7,000 hectares (ha). The average patch is less than four hectares. Only 3% exceed 20 ha, and the largest is 200 ha. Monsoon rainforest is composed of semi-deciduous or deciduous trees which lose their leaves towards the end of the dry season ("raingreen").
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.