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The extreme variations in rainfall are linked with the Australian-Indonesian monsoons.Generally speaking, there is a dry season (April to September), influenced by the Australian continental air masses, and a rainy season (October to March) that is caused by Asia and Pacific Ocean air masses.
Per the World Bank (2017) [1] [2]; Country mm/ year) Continent 1 Colombia 3,240: South America: 2 São Tomé and Príncipe 3,200: Africa Tuvalu 3,200: Oceania: 3 Papua New Guinea 3,142 ...
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]
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 Köppen climate classification is the most widely used climate classification system. [2] It defines a tropical climate as a region where the mean temperature of the coldest month is greater than or equal to 18 °C (64 °F) and does not fit into the criteria for B-group climates, classifying them as an A-group (tropical climate group). [3]
The Indramayu Regency has a tropical wet and dry Aw climate with two seasons, namely the rainy season and the dry season. The rainy season usually lasts from December to March. The dry season lasts from May to October. The average rainfall in the Indramayu Regency is 1300–1800 mm per year with the number of rainy days ranging from 90 to 140 ...
Indonesia's dry season will be less severe this year compared to 2023, improving its chances of managing forest fires and crops, the country's weather agency said on Friday. Last year's dry season ...
The rainy season occurs from September to February and it is a major source of energy for the Hadley circulation during boreal winter. It is associated with the development of the Siberian High and the movement of the heating maxima from the Northern Hemisphere to the Southern Hemisphere.