What is a Tropical Cyclone? Its Formation and Structure

A tropical cyclone looks a lot like a really large whirlpool that is found out in the tropics. It looks like a huge mass of air that just rotates, and while it does look like that- it isn’t really as much like the pictures make it out to be. In fact, they are really more disc like in shape than cyclonic.  When you look at them from space, you can really see a lot more about them, even though you can’t see their close details. Taking a look at how they are formed and their structure will give you more of an appreciation for this type of storm.

Tropical Cyclone Formation

Tropical cyclones are really a lot like a traveling source of heat. They feed on heat that is released from the moist air and condensation of the oceans.  Water temperature above 27 degrees is what required as tropical cyclones develop only over warm waters. As low-level winds flow into the group of thunderstorms over warm tropical waters, they evaporate water from the ocean surface. This process transfers energy from the ocean into the atmosphere. The winds rise up and release that energy into the air as they form clouds and precipitation. This warms the air and makes it almost like a hot air balloon, and encourages more warm air to flow in from the outside.

Tropical cyclones actually generate power, which gives them the ability to survive over the water. This is why they don’t usually make landfall, and when they do they don’t last for very long. They weaken tremendously after they hit land, because they depend on the moist air to be able to stay going strong. As temperature of water is not warm over higher altitudes, therefore cyclones do not form at higher altitudes. Most people think that a tropical cyclone is actually formed very quickly, but it starts out small, and then it begins to pick up energy as it goes.  It takes some time for it to fully strengthen to its full potential.

Structure of the Tropical Cyclone

The Eye of the Storm

If you have ever heard of the eye of the storm, then you are probably familiar with the fact that it is much like the center of the storm. The eye of the storm is actually where the storm is the most calm, but it doesn’t stay that way for very long.  When you venture out from the center of the storm, you will usually find it to be quite raging. The eye will usually be somewhere around 10 kilometers in diameter, and is the core of the storm.


Tropical cyclones are also made up of rainbands. These rainbands actually rotate and help the storm to circulate. They sweep through an area and can really wreak havoc. Most of the heavy rain that happens during a tropical cyclone will actually occur near the center of the storm, and outwards through the rainbands. Heavy precipitation can usually fall for hours during this type of storm, and it is usually due to these rainbands. As the center of the storm begins to approach, the rain and wind gusts will begin to pick up. The most heavy rainfall will occur just as the center of the storm begins to make landfall- if that even happens to begin with.


Next, you have the subsidence that comes from the rainbands. When rain falls from the tropical cyclone, it is fed back into the eye of the storm, and it begins to rotate back around. This is how it keeps going. To preserve the structure of the cyclone, you have to make sure that the forces are not disrupted. As the cyclone matures, it will actually have more and more subsidence.

Tropical cyclones can only be developed if the circumstances are favorable for the cyclone. If the circumstances are not where they should be, then the storm will just continue to decrease in weakness. As they first start out, they don’t develop further unless certain criteria are met. Once they are formed, they can last anywhere from a few days to a few weeks, depending on the conditions surrounding the storm. Not all of them will make it all the way to a full blown tropical cyclone, but some will. Only about half of them will actually make it all the way.

As you can see, there is a lot that goes into the formation and structure of a tropical cyclone. Most people will never experience this type of natural disaster, because they tend to stay out on the ocean. It is mainly the countries in the middle east and Asia that will actually have more experience with these storms. This is because they are much more prevalent there.

Consider yourself lucky if you haven’t found yourself in the midst of a tropical cyclone, because they can really cause a whole lot of damage. It really is a good thing that they are usually only found out in the oceans, because if they were to make landfall more often then they would likely cause a whole lot of damage that would be widespread throughout the world.

Image credit: NASA Goddard
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About Rinkesh

A true environmentalist by heart ❤️. Founded Conserve Energy Future with the sole motto of providing helpful information related to our rapidly depleting environment. Unless you strongly believe in Elon Musk‘s idea of making Mars as another habitable planet, do remember that there really is no 'Planet B' in this whole universe.