# Tropical cyclones in 2025

In 2025, tropical cyclones will form in seven major bodies of water, commonly known as tropical cyclone basins. Tropical cyclones will be named by various weather agencies when they attain maximum sustained winds of 35 knots (65 km/h; 40 mph). The strongest system this year so far is Cyclone Vince, which attained a minimum barometric pressure of 923 hPa (27.26 inHg), Cyclone Jude is the deadliest system this year so far, causing at least 21 deaths in south-east Africa. Cyclone Alfred is the costliest system this year so far at $759 million in damage. The accumulated cyclone energy (ACE) index for the 2025 (seven basins combined) so far, as calculated by Colorado State University (CSU), is 166.8 units overall.
Tropical cyclones are primarily monitored by ten warning centers around the world, which are designated as a Regional Specialized Meteorological Center (RSMC) or a Tropical Cyclone Warning Center ((TCWC) by the World Meteorological Organization (WMO). These centers are: National Hurricane Center (NHC), Central Pacific Hurricane Center (CPHC), Japan Meteorological Agency (JMA), Indian Meteorological Department (IMD), Météo-France (MFR), Indonesia's Meteorology, Climatology, and Geophysical Agency (BMKG), Australian Bureau of Meteorology (BoM), Papua New Guinea's National Weather Service (PNGNWS), Fiji Meteorological Service (FMS), and New Zealand's MetService. Unofficial, but still notable, warning centers include the Philippine Atmospheric, Geophysical and Astronomical Services Administration (PAGASA; albeit official within the Philippines), the United States's Joint Typhoon Warning Center (JTWC), and the Brazilian Navy Hydrographic Center.

## Systems
### January

In January, the Intertropical Convergence Zone (ITCZ), which allows for the formation of tropical waves, is located in the Southern Hemisphere, remaining there until May. This limits Northern Hemisphere cyclone formation to comparatively rare non-tropical sources. In addition, the month's climate is also an important factor. In the Southern Hemisphere basins, January, at the height of the austral summer, is the most active month by cumulative number of storms since records began. Of the four Northern Hemisphere basins, none is very active in January, as the month is during the winter, but the most active basin is the Western Pacific, which occasionally sees weak tropical storms form during the month. January was unusually active, with twelve systems forming and seven storms getting named.
The month started off in the South-West Indian Ocean with Cyclone Dikeledi, which intensified into a major cyclone before it made two landfalls at Antsiranana, Madagascar and Nampula Province, Mozambique, Cyclone Elvis and Cyclone Faida also formed but was downgraded into a depression by MFR in post-storm analysis. Meanwhile, short-lived Cyclone Pita formed on January 6, affecting some islands in the South Pacific basin. Weeks later, in the Australian basin, Cyclone Sean developed on January 17. Sean rapidly intensified into a Category 3-tropical cyclone, marking it the second major tropical cyclone of the year after Dikeledi. Cyclone Taliah and Cyclone Vince formed as well, with the latter rapidly intensifying into a Very Intense Tropical Cyclone in the South-West Indian Ocean, making it the strongest cyclone this month.

### February

February was extremely active. It was the most active month, and one of the third-most active months in any given year on record, with twelve systems forming and seven storms getting named. A total of seven tropical cyclones reached Category 3 strength or higher, the highest number since records began in 2003.
Historically, February is normally similar to January in terms of activity, with most formations being effectively restricted to the Southern Hemisphere (with the exception of the rare Western Pacific disturbance this year). The month also tends to see more strong tropical cyclones forming compared to January, despite seeing marginally fewer overall storms, due to the monsoon being at its height in the Southern Hemisphere. In the Northern Hemisphere, February is the least active month, with no Eastern or Central Pacific tropical cyclones and only one Atlantic tropical cyclone having ever formed in the month. Even in the Western Pacific, February activity is low: in 2025, the month never saw a typhoon-strength storm, the first being Typhoon Higos in 2015.
The month started off active with five systems forming in January and then persisting into February: Faida, 13U, Vince, Taliah, and 05F. Cyclone Zelia formed on February 7 near the Kimberley region, and rapidly intensified into a Category 5 severe tropical cyclone six days later; it then made landfall near De Grey in Australia as a Category 4 tropical cyclone. Two tropical cyclones formed in the Australian region on February 20 – Bianca and Alfred – while in the South-West Indian Ocean, two cyclones also formed near Madagascar: Garance and Honde. The former eventually became an intense tropical cyclone on February 27 before making landfall in the northern part of Réunion the next day as a slightly weaker tropical cyclone.

### March

During March, activity tends to be lower than in preceding months. In the Southern Hemisphere, the peak of the season has normally already passed, and the monsoon has begun to weaken, decreasing cyclonic activity, however, the month often sees more intense tropical cyclones than January or February. Meanwhile, in the Northern Hemisphere basins, sea surface temperatures are still far too low to normally support tropical cyclogenesis. The exception is the Western Pacific, which usually sees its first storm, often a weak depression, at some point between January and April.
Cyclone Alfred, Honde, and Garance formed in February and persisted into March. In March so far, three storms have formed, of which two have been named. The strongest storm of the month so far is Cyclone Jude, which made landfall in Madagascar and Mozambique, causing twenty-one deaths.

## Global effects

There are a total of seven tropical cyclone basins that tropical cyclones typically form in this table, data from all these basins are added.
| Season name | Season name | Areas affected | Systems formed | Named storms | Hurricane-force tropical cyclones | Damage (2025 USD) | Deaths |
| North Atlantic Ocean | North Atlantic Ocean | — | — | — | — | Un­known | — |
| Eastern and Central Pacific Ocean | Eastern and Central Pacific Ocean | — | — | — | — | Un­known | — |
| Western Pacific Ocean | Western Pacific Ocean | Vietnam, Malaysia, Singapore | 1 | — | — | Un­known | — |
| North Indian Ocean | North Indian Ocean | — | — | — | — | Un­known | — |
| South-West Indian Ocean | January – June | Madagascar, Mayotte, Mozambique, Comoros, Europa Island, Mascarene Islands, Île Amsterdam, Mauritius, Réunion | 5 | 4 | 3 | $170 million | 38 |
| South-West Indian Ocean | July – December | — | — | — | — | Un­known | — |
| Australian region | January – June | Broome, Port Hedland, Western Australia, Christmas Island, Cocos Islands, Queensland, Kimberley, Pilbara, Willis Island, New South Wales, Indonesia | 15 | 9 | 7 | Un­known | — |
| Australian region | July – December | — | — | — | — | Un­known | — |
| South Pacific Ocean | January – June | Tonga, Niue, Cook Islands, Samoa, Loyalty Islands, New Caledonia, French Polynesia, Vanuatu, Fiji, Wallis and Futuna | 6 | 2 | 2 | Un­known | — |
| South Pacific Ocean | July – December | — | — | — | — | Un­known | — |
| South Atlantic Ocean | South Atlantic Ocean | — | — | — | — | Un­known | — |
| Worldwide | Worldwide | (See above) | 26 | 16 | 12 | $929 million | 38 |
* 1 2 The wind speeds for this tropical cyclone/basin are based on the Saffir Simpson Scale which uses 1-minute sustained winds.
* 1 2 3 4 Only systems that formed either before or on December 31, 2025 are counted in the seasonal totals.
* ↑ The wind speeds for this tropical cyclone/basin are based on the IMD Scale which uses 3-minute sustained winds.
* 1 2 3 Only systems that formed either on or after January 1, 2025 are counted in the seasonal totals.
* ↑ The wind speeds for this tropical cyclone are based on Météo-France, which uses wind gusts.
* ↑ Although two systems formed in this basin, there are three named storms because after Tropical Low 08U moved into this basin, it was given a name, Dikeledi, by the MFR.
* ↑ According to the BoM, Cyclones Vince and Taliah entered the South-West Indian ocean basin from the Australian region
* ↑ According to the Bureau of Meteorology, Tropical Low 08U crossed directly into the Southwestern Indian Ocean on the evening of January 4 and was named Dikeledi three days later by Meteo France, which includes it in this category even though it was not named within the Australian region.
* ↑ The sum of the number of systems in each basin will not equal the number shown as the total. This is because when systems move between basins, it creates a discrepancy in the actual number of systems.