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Tropical cyclones in 2026

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  • 4 chapters
This map shows the tracks of all tropical cyclones in the 2026 Worldwide cyclone season . The points show the location of each storm at 6-hour intervals. The colour represents the storm's maximum sust
OreoStar-fait · Public domain

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Through Atmospheric pressure, China and El Niño–Southern Oscillation

Tropical cyclones are primarily monitored by 10 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.

Global atmospheric and hydrologic conditions

Global tropical cyclone activity during 2026 was shaped by a transition in the El Niño–Southern Oscillation (ENSO) phase. The year opened under weak-to-neutral La Niña conditions continuing from late 2025, which contributed to heightened tropical cyclone activity across the Southern Hemisphere basins—including the South-West Indian Ocean and Australian region—during January and February.

By mid-2026, sea surface temperature (SST) anomalies across the central and eastern equatorial Pacific indicated a rapid transition toward El Niño conditions. This warming trend suppressed early-season activity in the Atlantic basin, where high vertical wind shear led to a slow start with only two named tropical storms (Arthur and Bertha) forming through July. Conversely, the warming equatorial Pacific enhanced environmental conditions in the Eastern and Central Pacific and the Western Pacific, supporting rapid intensification events such as Super Typhoon Sinlaku in April and Major Hurricane Genevieve in July.

Sustained marine heatwaves across the Northern Hemisphere during the northern summer contributed to well-above-average sea surface temperatures in the Western Pacific and Northern Indian Ocean, fueling early basin activity and high accumulated cyclone energy (ACE) totals relative to long-term averages by midyear.

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