What Is a Tropical Cyclone?

What Is a Tropical Cyclone?

Weather Guide • Extreme Weather • 7 minute read

Rain bands Spiral arms of storms Eye Calm, clear centre Eyewall Strongest winds and rain Warm ocean water feeds the storm
A tropical cyclone seen from above: a calm eye, a ring of violent storms around it and spiral rain bands reaching far outward.

A tropical cyclone is a huge, rotating storm that forms over warm ocean water and can bring winds above 250 km/h, torrential rain and a wall of seawater onto the coast. Some are small and weak. The strongest are hundreds of kilometres wide and can affect millions of people. This guide explains what a tropical cyclone is, how it forms, what the different names mean and how to stay safe when one approaches.

The short answer: A tropical cyclone is a spinning storm system with a low-pressure centre, fed by heat and moisture from warm seas (about 26.5°C or more). Its winds spiral inward around a calm centre called the eye. It weakens quickly once it moves over cold water or land.

Tropical Cyclone, Hurricane and Typhoon: Same Storm, Different Names

These words describe the same type of storm. The name depends only on where it forms.

NameWhere it is used
HurricaneNorth Atlantic Ocean, Caribbean Sea and the northeast Pacific
TyphoonNorthwest Pacific, including Japan, China and the Philippines
CycloneArabian Sea, Bay of Bengal, South Pacific and Australian region

So a storm in the Arabian Sea that threatens Karachi or the Makran coast is called a cyclone, while the same kind of storm near Florida would be called a hurricane.

How Does a Tropical Cyclone Form?

A tropical cyclone needs several ingredients to come together at the same time. If one is missing, the storm usually fails to grow.

  • Warm ocean water: sea temperature of about 26.5°C or higher, reaching down roughly 50 metres. This is the fuel.
  • Moist air: humid air in the lower and middle atmosphere lets towering storm clouds keep growing.
  • Light upper-level winds: strong wind shear tears a young storm apart, so calm conditions are needed.
  • A starting disturbance: a cluster of thunderstorms or a low-pressure area to organise around.
  • Distance from the equator: the spin of the Earth (the Coriolis effect) is needed to make the storm rotate, so tropical cyclones almost never form within about 5 degrees of the equator.

Step by step

  1. Warm sea water heats the air above it, and the moist air rises.
  2. As the vapour rises and cools, it condenses into clouds and releases heat, which makes the air rise even faster.
  3. Air at the surface rushes in to replace it, and the Earth’s rotation twists this inflow into a spiral.
  4. The pressure at the centre keeps falling, the winds grow stronger and an eye can form.

Parts of a Tropical Cyclone

The eye

The eye is the centre of the storm, usually 30 to 65 kilometres wide. Skies can be clear and winds light. It can fool people into thinking the storm has ended, but the violent winds return from the opposite direction once the eye passes.

The eyewall

The eyewall is the ring of tall thunderstorms around the eye. It has the strongest winds and the heaviest rain in the entire cyclone.

Rain bands

Curved bands of showers and thunderstorms spiral outward from the centre. They can stretch far from the eye and bring gusts, heavy rain and even tornadoes long before the main part of the storm arrives.

Which Way Does It Spin?

In the Northern Hemisphere, a tropical cyclone rotates counter-clockwise. In the Southern Hemisphere, it rotates clockwise. Both are caused by the rotation of the Earth.

Stages and Strength of a Tropical Cyclone

A tropical cyclone grows through stages, based on its maximum sustained wind speed.

StageSustained wind speed
Tropical depressionBelow 63 km/h
Tropical storm63 to 118 km/h
Category 1 hurricane or typhoon119 to 153 km/h
Category 2154 to 177 km/h
Category 3 (major)178 to 208 km/h
Category 4 (major)209 to 251 km/h
Category 5 (major)252 km/h or more

These categories follow the Saffir-Simpson scale. Agencies in the North Indian Ocean use their own terms, such as cyclonic storm, severe cyclonic storm and very severe cyclonic storm, with slightly different wind thresholds. The category only measures wind. A weaker storm can still cause a disaster through rain or flooding.

Why Is a Tropical Cyclone So Dangerous?

Storm surge

The strong winds and the low pressure push the sea up and onto land as a wall of water. Storm surge is often the deadliest part of a tropical cyclone, especially along flat coastlines.

Destructive winds

Winds can tear off roofs, snap power poles, uproot trees and turn loose objects into flying debris.

Heavy rain and flooding

A slow-moving storm can drop huge amounts of rain. Flash floods and landslides can strike far inland, long after the winds have weakened.

Tornadoes

Rain bands can spawn short-lived tornadoes, mainly on the side of the storm where winds are strongest.

Where and When Do Tropical Cyclones Form?

Tropical cyclones form over warm tropical oceans. The main basins are the North Atlantic, the northeast and northwest Pacific, the North and South Indian Ocean and the Australian and South Pacific region. The Atlantic hurricane season officially runs from 1 June to 30 November. In the North Indian Ocean, activity peaks twice a year, before the monsoon (May and June) and after it (October and November).

Tropical Cyclones in Pakistan

Pakistan is not hit by cyclones as often as India or Bangladesh, but the risk is real. Storms form over the Arabian Sea and can threaten the coast of Sindh and Balochistan, including Karachi, Thatta, Gwadar and Ormara. Even when a cyclone does not make landfall, it can bring rough seas, strong winds, heavy rain, high tides and flooding. Cyclone Biparjoy in June 2023 is a recent example: it moved close to the Sindh coast, and thousands of people were moved to safer areas as a precaution. Fishermen are usually advised to stay out of the sea whenever a cyclone develops.

How Does a Tropical Cyclone End?

A tropical cyclone weakens when it loses its fuel. This happens when it moves over cold water, when it reaches land and loses the supply of warm moist air, or when strong wind shear breaks up its structure. A storm over land can still cause severe flooding for days, even after its winds have fallen.

Tropical Cyclone Safety Tips

  • Follow official warnings from your national weather service, such as the Pakistan Meteorological Department, and the instructions of local authorities.
  • Evacuate early if you are told to, especially if you live near the coast or in a low-lying area.
  • Prepare an emergency kit with drinking water, dry food, medicines, a torch, a power bank, a radio and copies of important documents.
  • Secure loose objects, shut windows and stay away from glass.
  • Do not go near the sea. Waves and surge can reach far beyond the beach.
  • Stay indoors, even if the eye passes over and it suddenly feels calm.
  • Never walk or drive through flood water.

For official forecasts and tracking maps, you can visit the National Hurricane Center. For updates in your area, check the live weather and weather maps on WeatherWorld.

Do Tropical Cyclones Get Names?

Yes. Naming storms makes warnings clearer and easier to remember, especially when more than one storm is active. Each region uses its own rotating lists of names agreed by the World Meteorological Organization. Names of especially deadly or costly storms are usually retired and never used again.

Is Climate Change Affecting Tropical Cyclones?

Research suggests that a warmer climate is making the strongest tropical cyclones more intense and increasing the amount of rain they produce. Rising sea levels also make storm surge more damaging. Scientists are less certain whether the total number of storms will change. This is an active area of study, and the details differ from one ocean basin to another.

Frequently Asked Questions

What is the difference between a tropical cyclone and a tornado?

A tropical cyclone is hundreds of kilometres wide, forms over the ocean and lasts for days. A tornado is only a few hundred metres wide, forms over land from a single thunderstorm and lasts for minutes.

Why is the eye of a tropical cyclone calm?

Air sinks in the centre of the storm, which warms and dries it and keeps clouds from forming. The strongest winds are in the eyewall just outside.

Can a tropical cyclone form on land?

No. It needs warm ocean water as fuel, so it dies out soon after moving inland.

How long does a tropical cyclone last?

Most last from several days to about two weeks, although some live longer if they stay over warm water.

Can we stop a tropical cyclone?

No. A strong one releases energy on a scale far beyond anything humans can control. The best defence is early warning, preparation and timely evacuation.

Final Thoughts

A tropical cyclone is one of the most powerful weather systems on Earth. It is born over warm seas, organised by the spin of the planet and carried toward land by the winds around it. Understanding how it forms and what it brings, from storm surge to flooding rain, helps you take warnings seriously and act early. Keep an eye on official forecasts during cyclone season, prepare before the storm approaches and never take a calm eye as a sign that the danger has passed.

Stay ahead of the storm: check the live weather, hourly forecast and weather maps on WeatherWorld.

What Is Atmospheric Pressure?

What Is Atmospheric Pressure?

Weather Guide • Everyday Science • 6 minute read

H High pressure Sinking air, clear skies 1013 hPa Air pressure at sea level Measured with a barometer L Low pressure Rising air, cloud and rain
Atmospheric pressure is the weight of the air above us, and it changes with height and weather.

You have never felt it as a weight, yet it is pressing on every centimetre of your body right now. Atmospheric pressure is so constant that we forget it exists, until we drive up a mountain and our ears pop, or until a weather forecaster says “falling pressure” just before a storm. This guide explains what it is, how it is measured and how a few simple readings can help you predict tomorrow’s weather.

The short answer: Atmospheric pressure is the force created by the weight of the air above a given spot. It is highest at sea level and falls as you climb. Changes in pressure over time are one of the most reliable early signs of a change in the weather.

Think of the Air as an Ocean

We live at the bottom of an ocean of air several hundred kilometres deep. Just as a diver feels more pressure at depth in the sea, we feel the combined weight of all the air stacked above us. Air seems weightless only because we are used to it. A large room contains many kilograms of it.

The reason we are not crushed is that the pressure inside our bodies pushes outward with the same force. The pressure is balanced from every side, so we never notice it.

How Pressure Is Measured

The most common unit in weather forecasts is the hectopascal (hPa), which is identical to the millibar. Average pressure at sea level is about 1013 hPa. Some countries use inches or millimetres of mercury, a unit that comes from the original barometer, which balanced a column of mercury against the weight of the air.

  • Mercury barometer: a tube of mercury whose height rises and falls with pressure.
  • Aneroid barometer: a sealed metal capsule that expands and contracts slightly. It is the type found in wall barometers and many instruments.
  • Electronic sensor: the tiny chip found inside most modern smartphones, watches and weather stations.

Why Pressure Falls as You Climb

The higher you go, the less air there is above you, so there is less weight pressing down. Pressure drops quickly at first. Around 5,500 metres up, it is about half of its sea-level value. This is why mountaineers struggle to breathe at great heights: the air contains the same share of oxygen, but each breath takes in fewer molecules.

Height above sea levelApproximate pressureExample
0 m1013 hPaKarachi coast
500 m955 hPaIslamabad area
2,000 m795 hPaMurree and the Galiyat
3,500 m655 hPaHigh mountain passes
5,500 m505 hPaBase camps of high peaks

These numbers are rough averages. Real values vary a little with the weather of the day.

Signs of Pressure in Daily Life

Your ears popping

When you drive uphill or take off in a plane, the pressure outside drops faster than the pressure behind your eardrum. The extra air inside pushes outward until a small tube in your ear lets it escape with a pop. Swallowing or yawning helps open that tube.

Water boiling at different temperatures

Water boils when its vapour pressure matches the pressure around it. Where the air pressure is lower, such as in the mountains, water boils at a lower temperature, so rice and lentils can take much longer to cook. A pressure cooker does the opposite. It traps steam, raises the pressure and lets food cook faster at a higher temperature.

Sealed packets that swell

A packet of chips sealed at sea level looks puffed up when you carry it to the hills, because the air inside pushes against the lower pressure outside. It is a quick, visible reminder of the pressure change.

Drinking through a straw

When you suck on a straw, you reduce the pressure inside it. The higher air pressure outside then pushes the drink up into your mouth. Strictly speaking, the atmosphere does the pushing, not your lungs.

Highs and Lows on the Weather Map

Air pressure is not the same everywhere. Weather maps mark areas of higher pressure with an H and areas of lower pressure with an L.

  • High pressure: air slowly sinks and warms, which prevents clouds from forming. Skies are usually clear and winds are light. In winter, clear nights under a high can feel very cold, and in some regions they bring fog or smog.
  • Low pressure: air rises and cools, so moisture condenses into clouds. Expect cloud, wind and rain. The deeper the low, the stronger the weather.

Wind itself is air moving from high pressure toward low pressure. The bigger the difference over a short distance, the stronger the wind.

How to Read the Pressure Trend Yourself

A single number does not tell you much, but the direction and speed of change do. Most weather apps show pressure under the details of the forecast. Check it every few hours and compare.

What the pressure is doingWhat it usually suggests
Rising slowly and steadilyImproving, settled weather
Rising quicklyClearing skies, often with gusty wind
SteadyNo big change soon
Falling slowlyClouds increasing, a change within a day
Falling quicklyStorm, strong wind or heavy rain approaching

As a rough guide, a drop of around 3 hPa or more in three hours is worth paying attention to. Treat the trend as a clue and not as a guarantee, and always use it alongside the forecast. If a fast fall is accompanied by darkening skies, read our guide on how to prepare for a thunderstorm.

Why Weather Services Use “Sea-Level Pressure”

A reading taken in a hill town would always look lower than one taken at the coast, simply because of height. To compare places fairly, meteorologists convert each reading to what it would be at sea level. That adjusted value is what you see on most forecasts and maps. If your own barometer or phone sensor shows a lower number than the forecast, the difference is probably just your altitude.

Pressure and the Seasons in Pakistan

Pakistan’s weather follows large pressure patterns. In early summer, intense heat over the plains creates a broad area of low pressure that pulls in moist air from the sea, helping to start the monsoon. In winter, higher pressure over the region brings dry, cool, settled days, interrupted when western disturbances, which are moving areas of low pressure, bring rain and mountain snow. Watching the pressure trend during these transitions gives a useful early hint of what is coming.

Does Pressure Affect How You Feel?

Some people say that changes in pressure bring on headaches or joint pain. Scientific studies have not settled this question, and results are mixed. If you notice a pattern in yourself, keep a simple diary and talk with a doctor if it troubles you. At high altitude, however, the effect of low pressure on the body is well documented: breathlessness, tiredness and headaches are common until you adjust.

Frequently Asked Questions

What is a normal pressure reading?

Around 1013 hPa at sea level. In real life, values normally fall between roughly 980 and 1040 hPa.

Does low pressure always mean bad weather?

Often, but not always. It makes cloud and rain more likely, but the amount of moisture and other factors also matter.

Can my phone measure pressure?

Many phones contain a barometer sensor, and some apps display the reading. It is good for watching trends.

Why is the pressure different in the hills?

There is less air above you at higher places, so there is less weight pressing down.

Final Thoughts

Atmospheric pressure is the weight of the air around us, invisible but always working in the background. It explains why your ears pop on a mountain road, why food cooks differently at altitude and why weather maps are filled with highs and lows. Learn to watch the trend, rising for improvement and falling for change, and you gain one of the oldest and simplest forecasting tools there is.

See what the air is doing: check the live weather, hourly forecast and weather maps on WeatherWorld.

What Is Atmospheric Pressure?

What Is Atmospheric Pressure?

Weather Guide • Everyday Science • 7 minute read

H High pressure Sinking air, clear skies 1013 hPa Air pressure at sea level Measured with a barometer L Low pressure Rising air, cloud and rain
Atmospheric pressure is the weight of the air above us, and it changes with height and weather.

You have never felt it as a weight, yet atmospheric pressure is pressing on every centimetre of your body right now. It is so constant that we forget it exists, until we drive up a mountain and our ears pop, or until a weather forecaster says “falling pressure” just before a storm. This guide explains what atmospheric pressure is, how it is measured and how a few simple readings can help you predict tomorrow’s weather.

The short answer: Atmospheric pressure is the force created by the weight of the air above a given spot. It is highest at sea level and falls as you climb. Changes in pressure over time are one of the most reliable early signs of a change in the weather.

Think of the Air as an Ocean

We live at the bottom of an ocean of air several hundred kilometres deep. Just as a diver feels more pressure at depth in the sea, we feel the combined weight of all the air stacked above us. Air seems weightless only because we are used to it. A large room contains many kilograms of it.

The reason we are not crushed is that the pressure inside our bodies pushes outward with the same force. The pressure is balanced from every side, so we never notice it.

How Atmospheric Pressure Is Measured

The most common unit in weather forecasts is the hectopascal (hPa), which is identical to the millibar. Average pressure at sea level is about 1013 hPa. Some countries use inches or millimetres of mercury, a unit that comes from the original barometer, which balanced a column of mercury against the weight of the air.

  • Mercury barometer: a tube of mercury whose height rises and falls with pressure.
  • Aneroid barometer: a sealed metal capsule that expands and contracts slightly. It is the type found in wall barometers and many instruments.
  • Electronic sensor: the tiny chip found inside most modern smartphones, watches and weather stations.

Pressure Units Compared

UnitStandard sea-level valueWhere it is used
Hectopascal (hPa) or millibar (mb)1013.25Most weather forecasts and maps worldwide
Kilopascal (kPa)101.3Science and engineering
Inches of mercury (inHg)29.92Aviation and weather reports in the United States
Millimetres of mercury (mmHg)760Medicine and older instruments

Why Atmospheric Pressure Falls as You Climb

The higher you go, the less air there is above you, so there is less weight pressing down. Pressure drops quickly at first. Around 5,500 metres up, it is about half of its sea-level value. This is why mountaineers struggle to breathe at great heights: the air contains the same share of oxygen, but each breath takes in fewer molecules.

Height above sea levelApproximate pressureExample
0 m1013 hPaKarachi coast
500 m955 hPaIslamabad area
2,000 m795 hPaMurree and the Galiyat
3,500 m655 hPaHigh mountain passes
5,500 m505 hPaBase camps of high peaks

These numbers are rough averages. Real values vary a little with the weather of the day.

Signs of Pressure in Daily Life

Your ears popping

When you drive uphill or take off in a plane, the pressure outside drops faster than the pressure behind your eardrum. The extra air inside pushes outward until a small tube in your ear lets it escape with a pop. Swallowing or yawning helps open that tube.

Water boiling at different temperatures

Water boils when its vapour pressure matches the pressure around it. Where the air pressure is lower, such as in the mountains, water boils at a lower temperature, so rice and lentils can take much longer to cook. A pressure cooker does the opposite. It traps steam, raises the pressure and lets food cook faster at a higher temperature.

Sealed packets that swell

A packet of chips sealed at sea level looks puffed up when you carry it to the hills, because the air inside pushes against the lower pressure outside. It is a quick, visible reminder of the pressure change.

Drinking through a straw

When you suck on a straw, you reduce the pressure inside it. The higher air pressure outside then pushes the drink up into your mouth. Strictly speaking, the atmosphere does the pushing, not your lungs.

Highs and Lows on the Weather Map

Air pressure is not the same everywhere. Weather maps mark areas of higher pressure with an H and areas of lower pressure with an L.

  • High pressure: air slowly sinks and warms, which prevents clouds from forming. Skies are usually clear and winds are light. In winter, clear nights under a high can feel very cold, and in some regions they bring fog or smog.
  • Low pressure: air rises and cools, so moisture condenses into clouds. Expect cloud, wind and rain. The deeper the low, the stronger the weather.

Wind itself is air moving from high pressure toward low pressure. The bigger the difference over a short distance, the stronger the wind.

The deepest lows of all belong to storms. A very fast fall in pressure is also a warning sign of a tropical cyclone approaching a coast.

How to Read the Pressure Trend Yourself

A single number does not tell you much, but the direction and speed of change do. Most weather apps show pressure under the details of the forecast. Check it every few hours and compare.

What the pressure is doingWhat it usually suggests
Rising slowly and steadilyImproving, settled weather
Rising quicklyClearing skies, often with gusty wind
SteadyNo big change soon
Falling slowlyClouds increasing, a change within a day
Falling quicklyStorm, strong wind or heavy rain approaching

As a rough guide, a drop of around 3 hPa or more in three hours is worth paying attention to. Treat the trend as a clue and not as a guarantee, and always use it alongside the forecast. If a fast fall is accompanied by darkening skies, read our guide on what a tornado is and how it forms.

Why Weather Services Use “Sea-Level Pressure”

A reading taken in a hill town would always look lower than one taken at the coast, simply because of height. To compare places fairly, meteorologists convert each reading to what it would be at sea level. That adjusted value is what you see on most forecasts and maps. If your own barometer or phone sensor shows a lower number than the forecast, the difference is probably just your altitude.

Atmospheric Pressure and the Seasons in Pakistan

Pakistan’s weather follows large pressure patterns. In early summer, intense heat over the plains creates a broad area of low pressure that pulls in moist air from the sea, helping to start the monsoon. In winter, higher pressure over the region brings dry, cool, settled days, interrupted when western disturbances, which are moving areas of low pressure, bring rain and mountain snow. Watching the pressure trend during these transitions gives a useful early hint of what is coming.

Does Pressure Affect How You Feel?

Some people say that changes in pressure bring on headaches or joint pain. Scientific studies have not settled this question, and results are mixed. If you notice a pattern in yourself, keep a simple diary and talk with a doctor if it troubles you. At high altitude, however, the effect of low pressure on the body is well documented: breathlessness, tiredness and headaches are common until you adjust.

Learn More

For a clear official explanation of how pressure shapes the weather, visit the National Weather Service JetStream guide to air pressure. To see how pressure and moisture work together, read how a rainbow forms, and to see how it affects the air you breathe, read what air quality is and how weather affects it.

Frequently Asked Questions

What is a normal atmospheric pressure reading?

Around 1013 hPa at sea level. In real life, values normally fall between roughly 980 and 1040 hPa.

Does low pressure always mean bad weather?

Often, but not always. It makes cloud and rain more likely, but the amount of moisture and other factors also matter.

Can my phone measure atmospheric pressure?

Many phones contain a barometer sensor, and some apps display the reading. It is good for watching trends.

Why is the pressure different in the hills?

There is less air above you at higher places, so there is less weight pressing down.

Final Thoughts

Atmospheric pressure is the weight of the air around us, invisible but always working in the background. It explains why your ears pop on a mountain road, why food cooks differently at altitude and why weather maps are filled with highs and lows. Learn to watch the trend, rising for improvement and falling for change, and you gain one of the oldest and simplest forecasting tools there is.

See what the air is doing: check the live weather, hourly forecast and weather maps on WeatherWorld.