Learn about tropical cyclones, how they form and whether they're the same as hurricanes, typhoons and tornadoes.
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Tropical cyclones are low pressure systems that form over warm tropical waters. They typically form when:
Tropical cyclones can continue for many days, even weeks. They may follow quite erratic paths.
A tropical cyclone often loses energy and breaks up when it moves:
In the Australian region, a tropical cyclone is defined as:
Organised convection means an area of thunderstorm activity associated with and organised around the low pressure system.
Mean wind speed is the speed of the wind, averaged over a 10-minute period at a given point.
For a tropical cyclone to form, it needs certain conditions and goes through stages as it develops.
The ocean water must be at least 26.5 °C. This heat fuels the developing tropical cyclone.
Tropical cyclones begin as weak circulations called 'tropical lows' – low pressure systems. Despite lower wind speeds than cyclones, tropical lows can still bring powerful thunderstorms and lots of rain.
A low pressure system is an area where the air pressure is lower than surrounding areas. Over the ocean, these systems cause warm, moist air to rise.
As the warm, moist air rises, the developing tropical cyclone begins to spin. See How cyclones spin on this page.
When there is a cluster of thunderstorms over a warm tropical ocean in an area of low pressure, they can form a band and start rotating around the low pressure area. In the right conditions, the cluster can grow and sustain itself.
As the storm rotates, it begins to draw in more warm, moist air. This comes from evaporation from the sea or is pulled in at low levels by the wind. This air rises and cools, causing clouds to form.
As the air nears the centre, it spins faster. The winds become stronger, drawing in air more quickly.
Some of the heavier, cool air sinks into the low pressure region at the centre of the tropical cyclone. This creates the relatively calm eye.
The eye is usually about 40 km wide but can range from 10 km to more than 100 km. It has light winds and often clear skies.
Rotating thunderstorms form spiral rainbands around the eye. The strongest winds and heaviest rain are found around the eye wall.
The low becomes a tropical cyclone when the wind speed is 63 km/h or greater, more than halfway around the centre. The new cyclone is given a name. View our Naming tropical cyclones page.
A tropical cyclone can maintain its structure while environmental conditions support it.
Tropical cyclones need a little help to start spinning. This mostly comes from forces created by the Earth turning on its axis.
A cyclone forms in an area of low pressure. This area of low pressure draws in surrounding winds. As the Earth rotates, it creates forces that cause the winds to swirl around the low pressure. This helps the cyclone start to spin.
To have a good chance of developing, a tropical low needs to be far enough away from the equator – usually at least 500 km.
This is because the forces created by the Earth's rotation are weaker near the equator and get stronger towards the poles. A tropical low near the equator is unlikely to get enough of a push to spin.
It is possible for a tropical cyclone to form on or near the equator if there is enough push from the wind. Such systems are rare and tend to be short-lived.
Tropical cyclones turn in different directions north and south of the equator. They spin:
This is due to the Coriolis effect.
The terms 'hurricane' and 'typhoon' are regionally specific names for a tropical cyclone.
The tropical cyclone season in Australia is officially between 1 November and 30 April.
Hurricanes and typhoons typically develop at different times of the year.
Tornado and twister are not the same as tropical cyclones.
Unlike a tropical cyclone, a tornado or twister:
Learn more about tornadoes.
See our Tropical cyclone forecast page.