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ORLANDO, Fla. — We’re just 100 days away from the start of the Atlantic hurricane season and while the Atlantic remains quiet right now, it could be quieter later this year for a whole different reason.
To understand why this year could be a quieter hurricane season, you must first understand ENSO – or the El Niño Southern Oscillation. It’s a climate index that monitors fluctuations of water temperatures in key areas of the Pacific basin.
What You Need To Know
- La Niña continues in the Pacific with an expected end by this Spring
- NOAA forecasts El Niño could develop by the peak of hurricane season
- This could become the first strong El Niño since 2023 to develop
- El Niño typically makes the Atlantic more hostile for hurricane development
There are three key states of ENSO – El Niño, La Niña and Neutral. They all signal a different temperature pattern in the Pacific basin, which can influence not only tropical patterns in the Atlantic, but globally.
It works like this: things that are warm like to rise, while things that are cold like to sink. And this rising and sinking motion works in tandem between the atmosphere and ocean.
So, when the Pacific basin warms up more than it should, it helps to promote rising air over the Pacific Ocean. Rising air helps to develop clouds and thunderstorms, which, if conditions are right, can further develop into a tropical system. This is known as El Niño.
Conversely, when the Pacific is colder than it should be, it promotes sinking motions. This sinking motion in the atmosphere helps to suppress rising motion, making it tougher for clouds and thunderstorms to form, and consequently harder for tropical systems to develop. This is known as La Niña.
When the Pacific basin is near its normal temperature state, we call this ENSO Neutral. Neutral states don’t typically have a big push one way or the other in supporting or suppressing tropical development.
How does this Pacific index drive Atlantic development?
ENSO may be measured in the Pacific Basin, but it has impacts across the global tropical pattern. When rising or sinking motions are set up in the Pacific basin, the opposite sets up in adjacent basins.
It’s just like the saying: what goes up, must come down.
So, when La Niña gets declared in the Pacific basin, that typically means rising motion is supported in the Atlantic basin, allowing for more clouds and thunderstorm development. While this doesn’t solely mean hurricane development is more likely, it is a key factor in helping to enhance the total storm count for the season.
Conversely, when El Niño gets declared in the Pacific – like we expect to happen this year – the rising motion moves to the Pacific basin. This should lead to sinking air across the Atlantic basin, which not only causes enhanced wind shear, but limits upward movement, which can reduce cloud and thunderstorm development. We typically see reduced storm count in these years as a result.
When does El Niño arrive?
According to the February report put out by the Climate Prediction Center last week, NOAA suspects the ongoing La Niña will come to an end by March or April. As the Pacific basin returns to a neutral state.
A growing pool of very warm water near Papua New Guinea and the Philippines should continue its trek eastward over the late Spring and early Summer months, gradually warming the east Pacific waters up further. The waters should reach a state of El Niño by the peak of hurricane season – which is between the middle of August to the middle of October.
This means while the start of the 2026 Atlantic Hurricane Season isn’t expected to see much of an influence from ENSO, the back half of the season might. Remember, ENSO patterns alone do not drive how a hurricane season could go. It’s just one piece of the puzzle, but it can be a big piece.
As we near the upcoming hurricane season, your Weather Experts will share tips and tricks to getting you hurricane ready. Remember, it only takes one storm to make it a bad season.
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Meteorologist Zach Covey
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