Category ‘6’ tropical cyclone hot spots are growing
Climate change is making massive hurricanes and typhoons more likely in the western Pacific, North Atlantic and Gulf
NEW ORLEANS — The oceanic conditions that churn up the very strongest of hurricanes and typhoons are heating up in the North Atlantic and Western Pacific, fueled by warm water that extends well below the surface. Human-caused climate change may be responsible for up to 70% of the growth of storm-brewing hotspots there, according to new research.
These hot spots are making it more likely that stronger Category ‘6’ tropical cyclones may hit landfall in highly populated areas.
“The hot spot regions have expanded,” said I-I Lin, a chair professor in the Department of Atmospheric Science at the National Taiwan University.
Lin will present the findings during an oral session on tropical cyclones at AGU’s 2025 Annual Meeting in New Orleans, Louisiana, on Wednesday, 17 December. From 15-19 December, AGU25 brings together more than 20,000 scientists to discuss the latest in Earth and space science research.
Lin has been interested in the strongest hurricanes and typhoons for more than a decade. Typhoon Haiyan—also known as Super Typhoon Yolanda—struck the Philippines at maximum intensity in November 2013, killing thousands of people. The next year, Lin and her colleagues published a paper calling for the need for creating a new category of tropical cyclones—6—for the very strongest storms like Haiyan, in the AGU journal Geophysical Research Letters.
Category 6 tropical cyclones would include those that exceed a wind intensity of 160 knots, Lin and her colleagues argue. Previously, any storm with winds above 137 knots were considered Category 5—most official weather agencies still recognize Category 5 tropical cyclones as the strongest. But since most other categories include a window of about 20 knots, Lin said it makes sense to create a Category 6. Category 4, for example, includes storms with wind intensity of 114-137 knots.
Some of the best-known of these storms include Hurricane Wilma in 2005, the most intense hurricane recorded in the Atlantic basin, Typhoon Haiyan and Typhoon Hagibis, which struck Tokyo in 2019. The latter was among the costliest in terms of destruction from rain and wind, Lin said, even though it had downgraded in intensity by the time it hit the Japanese capital. Finally, Hurricane Patricia, which formed in the Pacific Ocean off the coast of Mexico, was the strongest tropical cyclone ever recorded, with wind intensity of up to 185 knots—enough to make it considered a Category 7 storm, if such a thing existed, Lin said. “Patricia was the king of the world,” she added.
Burgeoning ocean hotspots feed big storms
Lin and her colleagues looked back at all large storms recorded in the past four decades or so, and found that these Category ‘6’ storms are increasingly common. In three decades from 1982 to 2011, there were eight tropical cyclones that had wind intensity of more than 160 knots. In the more recent decade she examined, from 2013 to 2023, there were 10 Category 6 tropical cyclones. So, of 18 Category ‘6’ cyclones that occurred the past 40 years or so, 10 of them happened in the last decade.
Lin’s ongoing recent work, the topic of her discussion at the upcoming session in the American Geophysical Union’s 2025 Annual Meeting, reveals that most of these Category ‘6’ tropical cyclones occur in hot spots. The largest hot spot for these massive storms is in the Western Pacific east of the Philippines and Borneo, while another hot spot lies in the North Atlantic around and to the east of Cuba, Hispaniola and Florida.
Their work also reveals that these hot spots are growing in size—the North Atlantic hot spot has expanded eastwards past the northern coast of South America and westwards into much of the Gulf, while the Western Pacific has grown as well.
The conditions that drive Category ‘6’ storms are driven by warmer subsurface water as well as warm surface water. In other regions, big storms often churn up the ocean. As cool water is drawn into the surface, it can cool the storm itself, reducing its intensity. But since warm water is so deep in these hot spot regions, the cyclones don’t have a chance to cool as much. Just the same, Lin cautions that not every storm that arises in these hot spots will become a Category ‘6’ tropical cyclone—the atmospheric conditions have to be right as well. “The hot spots are a necessary but not sufficient condition,” she said.
Analysis of the factors driving this expansion of deeper warm water in these hot spots has revealed that global warming and natural variability in temperature both play a role. But overall, the team estimates that human-caused climate change is responsible for about 60-70% of the increased size in these hot spots—and consequently, of Category ‘6’ tropical cyclones.
Lin said that recognition of Category ‘6’ tropical cyclones by weather agencies could help cities plan more appropriately for the impact of coming storms—especially in hot spot areas where they are becoming more common. “We really think there is a need just to provide the public with more important information,” Lin said.
Contributed by Joshua Rapp Learn
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Abstract information:
A31A-06 Category ‘6’ Tropical Cyclone Hot Spots in the Warming Climate
Wednesday, 17 December, 9:34 – 9:45 Central Time
Room 278-279 (NOLA Convention Center)
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Sri Lanka plans $1.6 bn in cyclone recovery
spending in 2026
Colombo (AFP) – Sri Lanka's government announced plans on Thursday for $1.6 billion in extra spending in 2026 to fund the country's recovery from Cyclone Ditwah, which killed more than 640 people.
Issued on: 18/12/2025 - RFI
The natural disaster affected 2.3 million people, more than 10 percent of Sri Lanka's population, and floods and landslides caused by the cyclone left extensive damage throughout the country.
The government convened parliament on Thursday, interrupting a month-long recess, to discuss what President Anura Kumara Dissanayake has described as the most challenging natural disaster to hit the island.
Dissanayake presented a request for an additional 500 billion rupees ($1.66 billion) for rebuilding devastated homes, roads, bridges and railways, as well as for cash handouts to help people regain lost livelihoods.
"We need to allocate an additional 500 billion rupees for disaster relief and reconstruction over and above the money allocated for government spending in calendar 2026," Dissanayake told parliament.
The national assembly, where his party holds a more than two-thirds majority, is expected to approve the mini-budget on Friday.
However, Dissanayake said the government does not intend to raise its borrowing limit to meet the additional expenditure.
He previously said he was banking heavily on foreign grants, and the finance ministry on Wednesday announced that it would call an international donor conference early next month.
The government has already asked the International Monetary Fund (IMF) for $200 million from a rapid relief fund and has secured World Bank agreement to repurpose $120 million from an ongoing project for disaster recovery spending.
On Tuesday, Sri Lanka also secured a $200 million loan from the Asian Development Bank to finance water management, the first such funding since the cyclone.
The finance ministry said the funds would be used to complete a canal network in the North-Central Province (NCP), which was among the worst affected by flooding last month.
"The objective of the project is to enhance agricultural productivity, farmer incomes and climate resilience in the NCP," the ministry said in a statement.
The World Bank has said it is in the process of assessing the damage caused by the cyclone, while Colombo has said preliminary estimates suggest it may need up to $7 billion to rebuild.
The cyclone struck as the country was emerging from its worst ever economic meltdown in 2022, when it ran out of foreign exchange reserves to pay for essential imports such as food, fuel and medicines.
Following a $2.9 billion bailout from the IMF approved in early 2023, the country's economy has stabilised.
© 2025 AFP