STUDY: Hurricanes Shifting Farther South…

Global warming is slowly moving hurricane formation southward. (credit: NASA)
In a nutshell
- Since 1979, hurricane genesis locations have shifted about 5 degrees (345 miles) southward, increasing storm risks for the Caribbean and parts of North America.
- Climate change is driving this shift. Decreasing vertical wind shear, caused by a weakening north-south temperature gradient, is making the southern North Atlantic more favorable for hurricane formation.
- Areas between 10°-20°N, including the Caribbean, Central America, and northern South America, may see more frequent and intense hurricanes, requiring improved preparedness and adaptation strategies.
BEIJING — Climate change has been pushing weather patterns to extremes across the globe, but not all changes follow predictable patterns. While much attention has focused on how tropical storms might intensify or move poleward with warming temperatures, a new study from the Chinese Academy of Sciences reveals a surprising trend in the Atlantic Ocean: hurricane genesis is actually shifting southward, bringing greater risks major locations that may not be prepared for increased storm activity.
The analysis, published in the journal npj Climate and Atmospheric Science, shows a southward migration in the genesis location of Atlantic hurricanes since 1979. A hurricane’s genesis is the point at which a tropical disturbance strengthens into a full-fledged tropical cyclone. This is different than global trends observed in other ocean basins, where tropical cyclones typically show a poleward shift.
Many of the areas that now find themselves in the new hurricane hotspot include small island nations in the Caribbean, as well as parts of Central America and the southeastern United States. Unlike the U.S. Gulf Coast, which has spent decades investing in hurricane preparedness, many of these newly affected regions have fewer resources and less infrastructure to handle major storms. More frequent hurricanes could mean a higher risk of devastating storm surges, flooding, and economic losses.
The Southward Shift: A Closer Look
For a storm to be officially classified as a hurricane, it must have sustained winds of at least 64 knots (74 mph or 119 km/h). In recent decades, more of these hurricanes have been forming in the southern portion of the North Atlantic (10°-20°N), where their frequency has increased, while areas further north have seen slight decreases.

Tropical cyclones, including hurricanes, are among the most destructive natural disasters, causing severe economic losses and casualties due to their strong winds, heavy rainfall, and storm surges. As global temperatures rise, understanding how these storms form and evolve is critical for improving disaster preparedness and climate adaptation strategies.
The researchers identified a southward shift of 0.114 degrees latitude per year for hurricane genesis locations. For perspective, over the 43-year study period (1979-2022), this represents a cumulative shift of nearly 5 degrees southward or roughly 345 miles. Hurricanes are also forming further east than they did four decades ago, with a longitudinal shift of 0.218 degrees longitude per year.
Why Hurricane Genesis Is Moving South
Through analysis of atmospheric and oceanic conditions, the research team identified a key factor driving the southward shift: decreasing vertical wind shear in the southern portion of the North Atlantic. Vertical wind shear, the change in wind speed or direction with height, typically disrupts hurricane formation. When this shear decreases, conditions become more favorable for powerful storms to develop.
“Our findings suggest that the southward shift in hurricane formation is closely tied to changes in atmospheric conditions under global warming,” says lead study author Xi Cao, associate professor at the Institute of Atmospheric Physics, in a statement. “This shift could heighten the risk of hurricanes in low-latitude regions, posing greater threats to vulnerable island nations and coastal communities in North America.”

The cause of decreasing vertical wind shear lies in changing temperature patterns. The study found that the north-south temperature gradient in the atmosphere has weakened because the subtropical regions (15°-30°N) are warming faster than tropical regions near the equator. This differential warming reduces the temperature contrast that drives strong vertical wind shear.
While the entire atmosphere is warming, the rate of warming differs by latitude and altitude. In this case, the subtropics are experiencing enhanced warming in the upper troposphere, the layer of atmosphere extending up to about 12 miles above Earth’s surface.
The researchers link this amplified subtropical warming to increased static stability, which means the atmosphere is more resistant to vertical motion. As static stability increases, it can trap heat and enhance warming in specific atmospheric layers.
To ensure their findings weren’t simply the result of natural climate variability, the team examined data from 39 climate models. They compared historical simulations, which include both human and natural influences, with pre-industrial control simulations that exclude human factors. The vertical wind shear decrease over the tropical North Atlantic appeared only in the historical simulations, suggesting that human-induced climate change, not natural variation, is driving the observed trends.
Implications for Hurricane-Prone Regions
Why does this southward shift differ from global trends of poleward migration in other ocean basins? The answer lies in the unique combination of atmospheric conditions in the Atlantic. In other regions like the Eastern North Pacific and Southern Indian Ocean, the background wind patterns are different so that the same temperature-driven changes reinforce rather than counteract the existing wind shear patterns.
For islands and coastal areas in the southern North Atlantic, particularly those between 10° and 20°N latitude, hurricane risk is likely increasing. This includes much of the Caribbean, parts of Central America, and northern South America. Not only are more hurricanes forming in these regions, but the storms also maintain their southward bias throughout their lifecycle, including when they reach their maximum intensity.
This shifting storm pattern is especially concerning for areas that may have less robust infrastructure or fewer resources for hurricane preparedness and recovery compared to more frequently affected regions further north.
It has become more and more clear that tropical cyclone patterns won’t just get uniformly worse; they’ll redistribute risk in complex ways. For those living along the southern reaches of North America’s coastlines and throughout the Caribbean, this southward hurricane shift is a forecast worth preparing for.
Paper Summary
Methodology
The researchers tracked hurricane trends using the IBTrACS dataset, which records hurricane position and intensity at six-hour intervals. They focused on the hurricane season from June to November between 1979 and 2022—a period with reliable satellite data. For atmospheric conditions, they used ERA5 reanalysis data and the Extended Reconstructed Sea Surface Temperature dataset. They employed linear regression analysis and the Mann-Kendall test to confirm statistical significance and compared observations with 39 climate models to distinguish natural variability from human-caused climate factors.
Results
The study found a southward shift in Atlantic hurricane genesis at a rate of 0.114 degrees latitude per year and an eastward shift of 0.218 degrees longitude per year. The southern North Atlantic (10°-20°N) showed a significant increase in hurricane formation, with decreasing vertical wind shear identified as the primary facilitating factor. This decreasing wind shear resulted from a weakening north-south temperature gradient due to faster warming in subtropical regions. The changes appeared only in climate model simulations that included human influences, not in pre-industrial control simulations.
Limitations
While hurricane data since 1979 is more reliable due to satellite coverage, this relatively short period limits confidence in long-term trend analyses. The results may be sensitive to the specific time period chosen. The study found clear trends for hurricanes but no significant shift for weaker tropical storms, suggesting complex relationships between storm intensity and migration patterns. Future projections using high-resolution climate models through 2050 showed no significant continuation of the southward trend, indicating uncertainty in how these patterns might evolve with further warming, though additional research is needed.
Funding and Disclosures
The research was supported by multiple Chinese scientific institutions, including the National Key R&D Program of China, the National Natural Science Foundation of China, and the Key Laboratory of South China Sea Meteorological Disaster Prevention and Mitigation of Hainan Province. The authors declared no competing interests. The study was a collaborative effort with scientists from multiple Chinese research institutions, the University of New South Wales in Australia, and other centers.
Publication Information
The study, “The southward shift of hurricane genesis over the northern Atlantic Ocean,” was published in npj Climate and Atmospheric Science (Volume 8, Article 37) on January 30, 2025. The research was led by Xi Cao, an associate professor at the Institute of Atmospheric Physics of the Chinese Academy of Sciences, and other international colleagues.