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Um ciclone tropical da região da Austrália … Um ciclone tropical da região da Austrália é um sistema não frontal de baixa pressão que se desenvolveu em um ambiente de altas temperaturas da superfície do mar e pouco vento vertical no Oceano Índico Meridional ou no Oceano Pacífico Sul. Dentro do hemisfério sul, existem oficialmente três áreas onde os ciclones tropicais se desenvolvem em uma base regular, essas áreas são o sudoeste do Oceano Índico entre a África e 90 ° E, a região australiana entre 90 ° E e 160 ° E e a bacia do Pacífico Sul entre 160 ° E e 120 ° W. A região australiana entre 90 ° E e 160 ° E é oficialmente monitorada pelo Australian Bureau de Meteorologia, a Indonésia Agência Meteorológica, Climatológica e Geofísica da Indonésia e o Papua New Guinea National Weather Service e, enquanto outros, como o Serviço Meteorológico de Fiji e a Administração Oceânica e Atmosférica Nacional dos Estados Unidos também monitora a bacia. Cada ano de ciclone tropical nesta bacia começa em 1 de julho e ocorre durante todo o ano, abrangendo a temporada de ciclones tropicais que vai de 1 de novembro e dura até 30 de abril de cada temporada. Na bacia, a maioria dos ciclones tropicais tem as suas origens na zona de convergência do Pacífico Sul ou no vale das monções do norte da Austrália, ambos formando uma extensa área de nebulosidade e são características dominantes da temporada. Dentro desta região, uma perturbação tropical é classificada como um ciclone tropical, quando tem velocidades de vento sustentadas de 10 minutos de mais de 65 km/h (40 mph), que envolve a meio caminho ao redor do centro de circulação de baixo nível, enquanto um ciclone tropical severo é classificado quando as velocidades máximas do vento sustentado de 10 minutos são superiores a 120 km/h (75 mph).inutos são superiores a 120 km/h (75 mph).
, An Australian region tropical cyclone is a … An Australian region tropical cyclone is a non-frontal, low-pressure system that has developed within an environment of warm sea surface temperatures and little vertical wind shear aloft in either the Southern Indian Ocean or the South Pacific Ocean. Within the Southern Hemisphere there are officially three areas where tropical cyclones develop on a regular basis: the South-West Indian Ocean between Africa and 90°E, the Australian region between 90°E and 160°E, and the South Pacific basin between 160°E and 120°W. The Australian region between 90°E and 160°E is officially monitored by the Australian Bureau of Meteorology, the Indonesian Meteorology, Climatology, and Geophysical Agency, and the Papua New Guinea National Weather Service, while others like the Fiji Meteorological Service and the United States National Oceanic and Atmospheric Administration also monitor the basin. Each tropical cyclone year within this basin starts on 1 July and runs throughout the year, encompassing the tropical cyclone season, which runs from 1 November and lasts until 30 April each season. 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 sustained wind speeds of more than 65 km/h (35 mph) that wrap halfway around the low level circulation centre, while a severe tropical cyclone is classified when the maximum 10-minute sustained wind speeds are greater than 120 km/h (75 mph).speeds are greater than 120 km/h (75 mph).
, 澳洲地區熱帶氣旋，是指在一季內，於赤道以南及90°E以東至160°E以西的澳洲地區水域，所產生的熱帶氣旋的一段時間，可說是風季的一種。雖然現時各氣象台並沒有定下任何熱帶氣旋季的指定期限，但大部份於南太平洋的熱帶氣旋通常都會於十一月至翌年四月期間形成。
, Siklon Tropis Wilayah Australia merupakan … Siklon Tropis Wilayah Australia merupakan sistem tekanan rendah non-frontal yang tumbuh pada lingkungan permukaan laut bersuhu hangat dan Geser angin yang rendah di atas Samudra Hindia bagian selatan dan selatan Pasifik. Daerah pertumbuhan siklon tropis wilayah Australia meliputi wilayah selatan khatulistiwa antara 90°BT hingga 160°BT. Daerah pertumbuhan siklon tropis ini secara resmi berada di bawah pengawasan dan pemantauan Badan Meteorologi Australia, BMKG Indonesia, dan Pusat Pelayanan Klimatologi dan Meteorologi Papua Nugini. Musim pertumbuhan siklon tropis di daerah ini berawal sejak 1 November hingga 30 April, tetapi banyak siklon tropis yang sudah terbentuk di wilayah ini bahkan sejak tanggal 1 Juli yang bukan merupakan musim pertumbuhan siklon tropis wilayah ini. Di daerah pertumbuhan siklon tropis ini, rata-rata siklon tropis terbentuk sebagai akibat dari Zona Konvergensi Pasifik Selatan dan pergerakan angin muson di selatan Indonesia dan utara wilayah Australia, sehingga menyebabkan terbentuknya area berawan yang sangat luas. Pada basin ini, gangguan tropis (tropical disturbance) sudah dianggap sebagai siklon tropis ketika kecepatan angin sepuluh menit memiliki kecepatan lebih dari 65 km/jam dan menyelimuti separuh jalur di sekitar pusat sirkulasi tingkat rendah. Sedangkan, siklon tropis yang kuat hingga sangat kuat terjadi ketika kecepatan angin sepuluh menit mempunyai kecepatan lebih dari 120 km/jam.mempunyai kecepatan lebih dari 120 km/jam.
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澳洲地區熱帶氣旋，是指在一季內，於赤道以南及90°E以東至160°E以西的澳洲地區水域，所產生的熱帶氣旋的一段時間，可說是風季的一種。雖然現時各氣象台並沒有定下任何熱帶氣旋季的指定期限，但大部份於南太平洋的熱帶氣旋通常都會於十一月至翌年四月期間形成。
, Um ciclone tropical da região da Austrália … Um ciclone tropical da região da Austrália é um sistema não frontal de baixa pressão que se desenvolveu em um ambiente de altas temperaturas da superfície do mar e pouco vento vertical no Oceano Índico Meridional ou no Oceano Pacífico Sul. Dentro do hemisfério sul, existem oficialmente três áreas onde os ciclones tropicais se desenvolvem em uma base regular, essas áreas são o sudoeste do Oceano Índico entre a África e 90 ° E, a região australiana entre 90 ° E e 160 ° E e a bacia do Pacífico Sul entre 160 ° E e 120 ° W. A região australiana entre 90 ° E e 160 ° E é oficialmente monitorada pelo Australian Bureau de Meteorologia, a Indonésia Agência Meteorológica, Climatológica e Geofísica da Indonésia e o Papua New Guinea National Weather Service e, enquanto outros, como o Serviço Meteorológenquanto outros, como o Serviço Meteorológ
, An Australian region tropical cyclone is a … An Australian region tropical cyclone is a non-frontal, low-pressure system that has developed within an environment of warm sea surface temperatures and little vertical wind shear aloft in either the Southern Indian Ocean or the South Pacific Ocean. Within the Southern Hemisphere there are officially three areas where tropical cyclones develop on a regular basis: the South-West Indian Ocean between Africa and 90°E, the Australian region between 90°E and 160°E, and the South Pacific basin between 160°E and 120°W. The Australian region between 90°E and 160°E is officially monitored by the Australian Bureau of Meteorology, the Indonesian Meteorology, Climatology, and Geophysical Agency, and the Papua New Guinea National Weather Service, while others like the Fiji Meteorological Service and tlike the Fiji Meteorological Service and t
, Siklon Tropis Wilayah Australia merupakan … Siklon Tropis Wilayah Australia merupakan sistem tekanan rendah non-frontal yang tumbuh pada lingkungan permukaan laut bersuhu hangat dan Geser angin yang rendah di atas Samudra Hindia bagian selatan dan selatan Pasifik. Daerah pertumbuhan siklon tropis wilayah Australia meliputi wilayah selatan khatulistiwa antara 90°BT hingga 160°BT. Daerah pertumbuhan siklon tropis ini secara resmi berada di bawah pengawasan dan pemantauan Badan Meteorologi Australia, BMKG Indonesia, dan Pusat Pelayanan Klimatologi dan Meteorologi Papua Nugini. Musim pertumbuhan siklon tropis di daerah ini berawal sejak 1 November hingga 30 April, tetapi banyak siklon tropis yang sudah terbentuk di wilayah ini bahkan sejak tanggal 1 Juli yang bukan merupakan musim pertumbuhan siklon tropis wilayah ini. Di daerah pertumbklon tropis wilayah ini. Di daerah pertumb
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Ciclone tropical na região da Austrália
, Australian region tropical cyclone
, 澳洲地區熱帶氣旋季
, Siklon tropis wilayah Australia
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