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What is the difference between a hurricane, typhoon and cyclone?

A hurricane, a typhoon and a cyclone are the same kind of storm, and which name is used depends mainly on where it happens.

Updated 51 minutes ago4 min readVersion 2
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Covers: Explains that hurricanes, typhoons and cyclones are the same weather phenomenon—tropical cyclones—and covers how they are named by region, how they form, and how they are classified. Does not cover specific storm forecasts or safety advice.

Also answers: Are hurricanes and typhoons the same? · Why are tropical cyclones called different names? · Hurricane vs typhoon vs cyclone · What makes a storm a hurricane or typhoon?

a large storm moving across the sky over a body of water
Photo: Daniel Lerman

The short answer

Evidence-backed AI-prepared starting map

A hurricane, a typhoon and a cyclone are the same kind of weather system — a tropical cyclone — and the name used depends mainly on where it occurs. A tropical cyclone is a rapidly rotating storm system with a low-pressure area, a closed low-level atmospheric circulation, strong winds, and a spiral arrangement of thunderstorms producing heavy rain and squalls. A hurricane is a strong tropical cyclone in the Atlantic Ocean or northeastern Pacific Ocean; a typhoon is the same thing in the northwestern Pacific Ocean; in the Indian Ocean and South Pacific, comparable storms are called "tropical cyclones". The same system can also be labelled tropical storm, cyclonic storm, tropical depression, or simply cyclone depending on its strength.1

What this rests on4 independent sources
  • Evidence 16

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In brief

  1. Hurricane, typhoon and cyclone are regional names for the same phenomenon: a tropical cyclone.1

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  2. Hurricanes occur in the Atlantic and northeastern Pacific; typhoons in the northwestern Pacific; "tropical cyclones" in the Indian Ocean and South Pacific.1

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  3. They form over warm ocean water and draw energy from evaporation and the condensation of rising moist air.1

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  4. Around 80–90 named tropical cyclones form worldwide each year, over half reaching hurricane-force winds of 65 kn (120 km/h; 75 mph) or more.1

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  5. Research treats them as one global phenomenon: shared observational archives, AI forecasting with a lead-time advantage of a day or more, and global hazard maps for present and future climates.234

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At a glance

The picture in numbers

Live · updated just now

Buoy and satellite observations, 1985–2017

2,927 tropical cyclones

tropical cyclones in a global archive2

The evidence behind it

4 sources
  • Other studies and data3
  • Background1

Published in 2024 and 2026

Sources on this page by kind and year
SourceKindYear
A dataset of global tropical cyclone wind and surface wave measurements from buoy and satellite platforms.Other studies and data2024
Operational tropical cyclone forecasting with AI.Other studies and data2026
Tropical cyclone (Wikipedia)BackgroundUnknown
Global coastal wind hazard maps from the CHAZ tropical cyclone model.Other studies and data2026

The community around it

No one has added to this page yet. Firsthand experience, a newer study or a different reading of the numbers would show up here, credited to you.

What it means for you

Which fits you?

Pick the situation closest to yours. Each answer says what it rests on.

If you hear a storm called a hurricane, typhoon or cyclone and want to know if it's the same thing

it is the same phenomenon — a tropical cyclone — and the name reflects the ocean basin where it occurs: Atlantic and northeastern Pacific for hurricanes, northwestern Pacific for typhoons, Indian Ocean and South Pacific for "tropical cyclones".1

Evidence-backed

If you're trying to understand why these storms are studied together worldwide

they share the same physics — forming over warm water and drawing energy from evaporation and condensation — so observations, forecasts and hazard maps are built globally rather than per region.12

Evidence-backed

If you're interested in how far forecasting has come

an AI model evaluated on 2023–2025 storms gave track, intensity and wind-radius predictions with an average lead-time advantage of a day or more over leading operational models, and improved a consensus ensemble when included.3

Evidence-backed

If you need long-range risk information rather than a specific forecast

global coastal wind hazard maps from the CHAZ model provide intensity exceedance probabilities and return periods for a recent historical period, mid-century and end-of-century.4

Evidence-backed

The full story · 3 chapters

01

Same storm, different names

AI summary:Hurricane, typhoon and cyclone are regional names for one phenomenon, a tropical cyclone, and the same storm may also be labelled by its strength.

Evidence-backed

Evidence-backed: The distinction between a hurricane, a typhoon and a cyclone is one of geography and language, not of physics. All three refer to a tropical cyclone: a rapidly rotating storm system with a low-pressure area, a closed low-level atmospheric circulation, strong winds, and a spiral arrangement of thunderstorms that produce heavy rain and squalls. A hurricane is a strong tropical cyclone that occurs in the Atlantic Ocean or northeastern Pacific Ocean. A typhoon is the same thing occurring in the northwestern Pacific Ocean. In the Indian Ocean and South Pacific, comparable storms are referred to as "tropical cyclones". The same system may also be called a tropical storm, cyclonic storm, tropical depression, or simply cyclone depending on its location and strength.1

Evidence-backed

Evidence-backed: In modern times, on average around 80 to 90 named tropical cyclones form each year around the world, and over half of these develop hurricane-force winds of 65 kn (120 km/h; 75 mph) or more.1

02

How they form

AI summary:These storms form over warm ocean water and get their energy from evaporation and from moist air rising, cooling and condensing into clouds and rain.

Evidence-backed

Evidence-backed: Tropical cyclones typically form over large bodies of relatively warm water. They derive their energy through the evaporation of water from the ocean surface, which ultimately condenses into clouds and rain when moist air rises and cools to saturation.1

03

Observing and forecasting these storms

AI summary:Because the storms are one global phenomenon, observations, AI forecasting and long-range hazard maps are built and studied worldwide.

Evidence-backed

Evidence-backed: Because these storms are the same phenomenon worldwide, research and monitoring efforts are global. A single archive brings together buoy and satellite observations — from altimeters, scatterometers and radiometers — plus best-track estimates of storm tracks and wind-field parameters, covering 2,927 tropical cyclones worldwide from 1985 to 2017.2

Evidence-backed

Evidence-backed: Forecasting has advanced on the same global footing. An AI-based model (WN-C), evaluated on tropical cyclones from 2023 to 2025, produced track, intensity and wind-radius predictions with an average lead-time advantage of one day or more over leading operational models — an accuracy improvement comparable to a decade of operational development. It achieved this using inputs orders of magnitude coarser than regional models, and adding its predictions to a weighted-average consensus ensemble improved that ensemble's skill substantially. The approach scales to ensembles of up to 1,000 members, which capture rare events better than conventional 50-member ensembles.3

Evidence-backed

Evidence-backed: For longer-range risk assessment, synthetic tropical cyclone models are used because observational records are short and climate change is shifting the picture. Global coastal wind hazard maps built with the Columbia TC hazard model (CHAZ) cover a recent historical period (1995–2014), mid-century (2041–2060) and end-of-century (2081–2100), plus a reference dataset downscaled from an observation-based reanalysis for 1981–2019. These maps show storm intensity exceedance probabilities and return periods.4

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Quick questions from connected pages

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What to remember

Try to recall each hidden figure before you reveal it. Remembering, not rereading, is what makes it stick.

  1. Around named tropical cyclones form worldwide each year, over half reaching hurricane-force winds of 65 kn (120 km/h; 75 mph) or more.

  2. Hurricane, typhoon and cyclone are regional names for the same phenomenon: a tropical cyclone.

  3. Hurricanes occur in the Atlantic and northeastern Pacific; typhoons in the northwestern Pacific; "tropical cyclones" in the Indian Ocean and South Pacific.

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  1. 1
    Tropical cyclone (Wikipedia)
    WikipediaPublished Oct 10, 2026Checked Oct 10, 2026
    “A tropical cyclone is a rapidly rotating storm system with a low-pressure area, a closed low-level atmospheric circulation, strong winds, and a spiral arrangement of thunderstorms that produce heavy rain and squalls. Depending on its location and strength, a tropical cyclone is called a hurricane (), typhoon (), tropical storm, cyclonic storm, tropical depression, or simply cyclone. A hurricane is a strong tropical cyclone that occurs in the Atlantic Ocean or northeastern Pacific Ocean. A typhoon is the same thing which occurs in the northwestern Pacific Ocean. In the Indian Ocean and South Pacific, comparable storms are referred to as "tropical cyclones". In modern times, on average around 80 to 90 named tropical cyclones form each year around the world, over half of which develop hurricane-force winds of 65 kn (120 km/h; 75 mph) or more. Tropical cyclones typically form over large bodies of relatively warm water. They derive their energy through the evaporation of water from the ocean surface, which ultimately condenses into clouds and rain when moist air rises and cools to saturation.”
  2. 2
    A dataset of global tropical cyclone wind and surface wave measurements from buoy and satellite platforms.
    Scientific data (Tamizi & Young)Published Jan 22, 2024Checked Oct 10, 2026
    “There are now a range of potential data sources for wind and surface wave conditions within tropical cyclones. These sources include: in situ buoy data and remote sensing data from satellite altimeters, scatterometers, and radiometers. In addition, data providing estimates of tropical cyclone tracks and wind field parameters are available from best track archives. The present dataset brings together this information in a single archive, providing the available data for each tropical cyclone from each of the data sources in a single file. The data consists of observations in a total of 2927 global tropical cyclones over the period from 1985 to 2017. Global statistics of the observations are provided, along with data on the geographic distribution of tropical cyclones within the database.”
  3. 3
    Operational tropical cyclone forecasting with AI.
    Nature (Alet et al.)Published Aug 6, 2026Checked Oct 10, 2026
    “When evaluated on tropical cyclones from 2023 to 2025, the track, intensity and wind-radius predictions from WN-C offer an average lead-time advantage of 1 day or more over leading operational models-an improvement in accuracy comparable to the progress seen in the last decade of operational development. We achieved these results using inputs that are orders of magnitude coarser than regional models, suggesting that high resolution is not a strict prerequisite for state-of-the-art intensity forecasting and that these coarse atmospheric data contain more intensity signal than has been previously recognized. Including predictions from WN-C in a weighted-average consensus ensemble improves its skill substantially. The scalability of WN-C enables ensembles of up to 1,000 members, which are better at capturing rare events than conventional 50-member ensembles. By providing advanced operational ensemble guidance to human forecasters, this work represents a step change towards more reliable and timely forecasts and warnings that can help to protect lives and to mitigate the devastating effects of tropical cyclones.”
  4. 4
    Global coastal wind hazard maps from the CHAZ tropical cyclone model.
    Scientific data (Meiler et al.)Published Jan 17, 2026Checked Oct 10, 2026
    “Synthetic tropical cyclone (TC) models have become essential tools for assessing TC hazard and risk, due to both the shortness of observational records and, now, the influence of climate change. However, the direct output from these models, TC track sets, requires additional processing to become useful for impact assessments beyond traditional climate science and meteorological research. Converting TC tracks into hazard maps condenses complex information on TC intensity and frequency into widely accessible formats, facilitating diverse impact analyses. Here, we present global coastal wind risk maps generated using the Columbia TC hazard model (CHAZ) for both present-day and future climate conditions. Climate scenario-driven data are provided for a recent historical period (1995-2014) and two future periods, mid-century (2041-2060) and end-of-century (2081-2100); a reference data set downscaled from an observation-based reanalysis for 1981-2019 is also provided. These hazard maps depict TC intensity exceedance probabilities and return periods, providing valuable insights to policymakers, planners, and researchers focused on disaster preparedness.”

How it changed

Published 1 time since Oct 10, 2026.

  1. Version 2Oct 10, 2026Live now

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  • What wind-speed thresholds separate a tropical depression, tropical storm, hurricane and typhoon, and do these thresholds differ between the regional agencies that name storms?

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