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Tropical cyclone warning centres are located in these cities as they are the major centres along the coasts where most cyclones occur. Cyclones rarely hit as far south as Perth, but Perth is the capital of Western Australia, and the centre for communications - thus it is a logical location. Brisbane is in a similar situation. Darwin is right in the middle of cyclone territory.

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COOL
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Anonymous

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well it boring too :}
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nioce
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Very useful info
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Q: Why are the Tropical Cyclone Warning centers located in Perth Darwin or Brisbane?
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Others form when other types of cyclones acquire tropical characteristics. Tropical systems are then moved by steering winds in the troposphere; if the conditions remain favorable, the tropical disturbance intensifies, and can even develop an eye. On the other end of the spectrum, if the conditions around the system deteriorate or the tropical cyclone makes landfall, the system weakens and eventually dissipates. It is not possible to artificially induce the dissipation of these systems with current technology. Part of a series onTropical cyclonesFormation and namingDevelopmentStructureNamingList of storm namesEffectsWarnings and watchesStorm surgeNotable stormsClimatology and trackingBasinsRSMCsScalesObservationForecastingRainfall forecastingRainfall climatologyHistoric listshistoricList of retired Atlantic hurricane namesList of retired Pacific hurricane namesList of retired Pacific typhoon names (JMA)List of named tropical cyclonesList of historic tropical cyclone namesTropical cyclones portalv · d · eContents[hide] 1 Physical structure 1.1 Eye and center1.2 Size2 Mechanics3 Major basins and related warning centers4 Formation 4.1 Times4.2 Factors4.3 Locations5 Movement and track 5.1 Steering winds5.2 Coriolis effect5.3 Interaction with the mid-latitude westerlies5.4 Landfall5.5 Multiple storm interaction6 Dissipation 6.1 Factors6.2 Artificial dissipation7 Effects8 Observation and forecasting 8.1 Observation8.2 Forecasting9 Classifications, terminology, and naming 9.1 Intensity classifications 9.1.1 Tropical depression9.1.2 Tropical storm9.1.3 Hurricane or typhoon9.2 Origin of storm terms9.3 Naming10 Notable tropical cyclones11 Changes due to El Niño-Southern Oscillation12 Long-term activity trends13 Global warming14 Related cyclone types15 Tropical cyclones in popular culture16 See also17 References18 External linksPhysical structureSee also: Eye (cyclone)Structure of a tropical cycloneAll tropical cyclones are areas of low atmospheric pressure in the Earth's atmosphere. The pressures recorded at the centers of tropical cyclones are among the lowest that occur on Earth's surface at sea level.[1] Tropical cyclones are characterized and driven by the release of large amounts of latent heat of condensation, which occurs when moist air is carried upwards and its water vapor condenses. This heat is distributed vertically around the center of the storm. Thus, at any given altitude (except close to the surface, where water temperature dictates air temperature) the environment inside the cyclone is warmer than its outer surroundings.[2]Eye and centerA strong tropical cyclone will harbor an area of sinking air at the center of circulation. If this area is strong enough, it can develop into a large "eye". 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