Science Facts

How Cyclone Is Formed? – Causes, Types & Safety Tips


On the evening of November 12, 1970, the Bhola cyclone barreled up the Bay of Bengal. There were sustained winds of 240 kilometers per hour and a storm surge or flooding that raised the sea level to 10.4 meters. The damaging wind and flooding were devastating. And the Bhola cyclone is the deadliest tropical cyclone in history, killing an estimated 300,000 to 500,000 people.

Weather encapsulates all the atmospheric conditions in a specific place at a particular time. And if you live in the mid-latitudes, or everything roughly between 35 and 55 degrees north and south latitude, you can expect the weather to be predictably unpredictable. A bright sunny day in South Dakota or the South Island of New Zealand or Scotland can suddenly change to overcast and grey and then just as abruptly clear up.

There are so many complex global circulation patterns in the atmosphere and the oceans. The Earth is curved and tilted. The amount of incoming solar radiation, or insolation, isn’t the same everywhere. Each year, tropical regions receive two and a half times more energy than the poles. It has to be evened out with the help of circulation in the atmosphere.

How cyclone is formed?

Storm force winds, torrential rain, massive pressure falls, and storm surges are all produced simultaneously by the most deadly weather. Around the Indian Ocean and southeast Pacific, these massive storms are known as cyclones. Cyclones tend to affect countries like Madagascar, India, and parts of Australia. In the Northwest Pacific, tropical storms are known as typhoons.

There are three basic stages in the life of a tropical cyclone. Its origin or source is the mature stage and the dissipation stage, where it dies out. These occur in a continuous process, not as separate in distinct stages. Each stage may occur more than once during the life cycle. As the cyclone’s strength rises and falls, it may reach land weakened, then go back out to sea where it strengthens once more. The formation of a cyclone depends upon the following conditions coinciding.

Cyclone formation
Cyclone formation

The warm ocean area with a surface temperature exceeds 26.5 degrees Celsius over an extended period. It allows a body of warm air to develop above the ocean’s surface. Low altitude winds are also needed to form a tropical cyclone. As air warms over the ocean, it expands, becomes lighter, and rises. Other local winds blowing to replace the air that has risen have also warmed and rises.

The rising air contains vast amounts of moisture evaporated from the ocean’s surface. It cools, condensing to form huge clouds about ten kilometers up in the troposphere as it rises. More warm air rushes in and rises drawn by the draft above. The rising drafts of air carry moisture high into the atmosphere so that these clouds eventually become very thick and heavy.

Condensation then releases the latent heat energy stored in the water vapor providing the cyclone with more power. This creates a self-sustaining heat cycle. Drawn further upwards by the new release of energy, the clouds can grow to 12-15 kilometers high. The force is created by the Earth’s rotation on a tilted axis.

The Coriolis effect causes rising currents of air to spiral around the center of the tropical cyclone. It is at this stage that the cyclone matures, and the eye of the storm is created. As the air rises and cools, some of this dense air descends to form that still clear eye as the cyclone rages around it. The eyewall where the wind is strongest behaves like a whirling cylinder.

  • Cyclones rotate clockwise in the southern hemisphere, anti-clockwise in the northern.

The lowest air pressure in a tropical cyclone is always found at the center. And it is typically 950 millibars or less. The average air pressure at the Earth’s surface is about 1010 millibars. Tropical cyclones have significantly lower air pressure than the air that surrounds them. The bigger the pressure difference, the stronger the wind force.

One of the lowest air pressures ever recorded was 877 millibars. Typhoon Ida hit the Philippines in 1958, where winds reached 300 kilometers an hour. Once formed, the Cyclones movement or track follows a pathway away from its source driven by global wind circulation. As warm ocean waters feed it to heat and moisture, the cyclone continues to enlarge.

Scientific explanation: What are the causes of cyclones? Everything is in place, converging trade winds meet the warm air with water vapor rising. In the cooling, the air-water vapor condenses into droplets. This state change from water vapor to liquid releases latent heat, further warming the atmosphere and becoming more buoyant. The air rises even more rapidly and produces more and more violent thunder clouds. But that’s only the beginning.

Trade winds drawn in at the Earth’s surface arrive on a curved path due to the Earth’s rotation. As the storm grows larger, more moist warm air is drawn in at the surface. More water vapor condenses into cloud droplets, and more latent heat is released. This is how energy is driven into the storm, and the speed of rotation increases. This system is now a tropical storm.

When the surface wind reaches sustained speeds of over 74 miles an hour, the storm is officially a Category 1 hurricane. What’s happening inside the storm-rising currents of warm moist air from thunder clouds? As the air cools, it becomes denser and falls again. And we get this alternating pattern of storm clouds with clear slots in between. It gives us the appearance of spiraling rain bands.

As a hurricane grows in intensity, it develops a very distinctive structure with what looks like a hole in the middle of a swirling mass of clouds. This clear zone in the storm’s center is called the eye, and around it is the eyewall. The eyewall is the most destructive part of the hurricane containing the most severe thunderstorm
and the very strongest winds.

Types of cyclone

There are mainly two types of cyclones: tropical cyclones and temperate cyclones. These types of cyclones happen several times in a year for the region and temperature.

Tropical cyclones: A tropical cyclone is an area of low pressure that forms in tropical regions. They help essentially balance out the temperature across the globe. They take the heat energy from the tropics. The generic term is a tropical cyclone that can refer to any cyclone with a closed center of circulation globally, like in the Atlantic. When they get strong enough to a certain wind speed, we call them hurricanes.

Temperate cyclones: Airmasses are huge atmospheric volumes with particular temperature and humidity characteristics. When two different air masses come into contact, they don’t mix. They push against when a warm air mass meets a cold air mass. The warm air rises since it is lighter at high altitudes. It cools and the water vapor. It contains condenses. This type of front is called a warm front. It generates nimbostratus clouds which can result in moderate rain.

On the other hand, a cold air mass catches up with a warm air mass. The cold air slides under the warm air and pushes it upward. As it rises, the warm air cools rapidly. This configuration called a cold front gives rise to cumulonimbus clouds often associated with heavy precipitation and storms. As air masses move pushed by winds, they directly influence the weather in the regions they pass in this way. They help to circulate heat and humidity in the atmosphere.

Mid-latitude cyclones: The uneven amounts of insolation also cause temperature differences that drive some of the biggest rebalancing efforts. Mid-latitude cyclones, which are also called wave cyclones or extratropical cyclones. These enormous weather systems span 1000 kilometers or more. A mid-latitude cyclone is a relatively huge circular weather system. It is a relatively smaller, extremely windy tropical storm.

Mid-latitude cyclones can last a week or more, bringing many changes in the day-to-day weather or severe storms as they travel from west to east with the westerly winds. These weather systems can form in the mid-latitudes of both hemispheres. In the Northern Hemisphere, mid-latitude cyclones form along the polar front. It is a low-pressure band in the latitudes just below the poles between two large high-pressure areas.

  • The subtropical high pressure to the south and the polar high to the north.

A battle rages in the skies between the warm, moist air from the tropics and the poles’ cold air. The term “polar front” was first proposed by Norwegian meteorologists Jacob Bjerknes and Halvor Solberg. When an air mass forms over tropical oceans, it will be relatively warmer and more humid than one that forms over northern Canada’s frigid interior. It will be cold and very dry. And as they move, they bring their temperatures and moisture with them.

The mid-latitudes get a lot of clashes between air masses. A lot of the storms and precipitation come from because when different air masses come together. If the displaced warm air is unstable and has lots of moisture, we’ll get heavy rain from thunderstorms and an advancing wall of cumulonimbus clouds. But when a cold air mass backs off, the warm air mass sees its chance and creeps in, forming a warm front. The warm air can’t displace the denser, colder air near the ground.

The first sign of one is high cirrus clouds, followed by lower and thicker altostratus clouds. Then still lower and thicker stratus clouds that bring drizzly rain. Different air masses bring different weather in their wake and influence locations’ weather conditions as they pass. These winds blow very fast because there’s less friction higher up. And within the upper air westerlies about 10 kilometers above the Earth, there’s a wind that blows fast. It’s the polar front jet stream, and it travels up to 450 kilometers per hour.

As the air converging and rising to form a low-pressure area turns into a full-blown mid-latitude cyclone, the colder air mass is denser and moves faster. And it won’t be over until the cyclone is wholly cut off from the warm air mass, energy, and moisture source. A storm that starts in the tropical oceans between the Tropic of Cancer and the Tropic of Capricorn can grow to have incredible winds over 118 kilometers per hour. They go by many names: hurricanes in the Atlantic, typhoons in the Pacific, and cyclones in the Indian Ocean.

How to prepare for a cyclone?

To protect from cyclones, you need to follow some advice and safety tips. These can help to reduce the suffering rate. Here are some tips before the cyclones and during and after the cyclone.

Safety tips before the cyclone

  • Monitor the weather conditions from your local weather station through mainstream and social media.
  • Be informed at all times and make sure that the place you’re staying is capable of withstanding strong winds and heavy rains. It helps to check roofs for weeks and other parts of your house for damage.
  • Have your survival kit ready. This may include first-aid kits, flashlights, cellphone, batteries, whistles, power banks, and other essential items.
  • Make sure that enough source of drinking water.
  • Place pertinent documents and waterproof containers. Clothes should be placed in plastic bags.
  • Coordinate with local authorities for possible evacuation if advised to do. So never hesitate to evacuate when evacuating.
  • Switch off the primary power source of the house and unplug all electrical devices. Lock all doors and windows.
  • Don’t forget to bring money just in case during the storm.

Safety tips during the cyclone

  • Keep calm and stay indoors continuously.
  • Monitor the weather from your local weather station through mainstream and social media.
  • If electrical power is down, make use of battery-operated transistor radio to check the news.
  • Keep away from flooded areas unless you want to catch leptospirosis or fall into a maintenance hole.
  • Double-check the weather conditions.

It is important always to be ready for any situation.


Glossary of Meteorology. “Cyclonic circulation.” American Meteorological Society.
BBC Weather Glossary. “Cyclone.”
“UCAR Glossary — Cyclone.” University Corporation for Atmospheric Research.

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