Hurricane Season 2026 – What To Expect This Year

By WeatherFlow-Tempest Meteorologist Shea Gibson 

The 2026 Hurricane Season began on June 1st for the Atlantic basin. This year will uniquely  differ from the past recent years as we have a few factors that will limit development from the  beginning and through the bulk of the peak season. In this article, I will show you the hurricane  season forecast 2026 from both NOAA NHC and from Colorado State University, where think  tanks such as Phil Klotzbach adds valuable perspective to the tropics. I will also show some  visual information to help you understand why our ongoing Atlantic hurricane season prediction  will be different this year.  

As far as the official hurricane season forecast provided by NOAA/NHC on May 21, 2026, they are calling for a 55% chance for a below average season with 8-14 named storms, 3-6 hurricanes  and only 1-3 major hurricanes.  

Source: https://www.noaa.gov/news-release/noaa-predicts-below-normal-2026-atlantic hurricane-season

CSU issued their prediction earlier on April 9, 2026 and also agrees with a below average season  with 11 named storms, 5 hurricanes and only 2 major hurricanes.  

Source: https://tropical.colostate.edu/forecasting.html 

And here are the names as of June 20th, 2026, with Arthur already being used as a briefly lived,  weak tropical storm on Thursday, June 18, 2026.

To understand why the below average predictions are being issued, let’s first start with the  elephant in the room, which is the ENSO (El Niño Southern Oscillation) cycle that you’ve likely  been hearing about in various media outlets. This particular weather event stems from the  equatorial central Pacific, where a specific area called “Nino Region 3.4” is measured for sea  surface temperatures and atmospheric conditions and averaged over a three-month period to  tell us which phase of the ENSO we are in. If the surface waters in that area rise above 0.5°C  above normal for the three-month average along with relaxing of the Easterly trade winds, then  we go from Neutral (normal) to El Niño. Conversely, if it drops below -0.5°C with increased  Easterly trades, then we slide into a La Niña phase.  

Source: https://www.ncei.noaa.gov/access/monitoring/enso/sst 
Source: Tropical Tidbits with edits by WeatherFlow Meteorologists Shea Gibson https://www.tropicaltidbits.com/analysis/ocean/

The June 2026 update from the Climate Prediction Center put us in an El Niño based on current  observations – and we have an increasing probability to have a strong El Niño by late fall and  into winter 2026-2027. Just for reference, a strong El Niño is when those SST’s increase above  2.0°C above normal. What this means is that we have more buoyancy of air with more lifting,  and less upper shear over the eastern north Pacific, so they will have a very active year.  Meanwhile over the Atlantic basin, the Corolis effect pulls that air from west-to-east and creates a large pool of sinking air with lots of upper shear. This sinking air makes it difficult for tropical  cyclones to aggregate storms around a central core with the hinderance of vertical stacking.  Additionally, the upper shear tears cloud-tops off as storms try to stack vertically and are blown away from over the core. In short, these two key factors make for large areas of hostile  environments where tropical systems would normally form.  

Source: https://cpc.ncep.noaa.gov/products/analysis_monitoring/enso/roni/strengths/ 

As far as the start of the season as El Nino is just getting cranked up, another factor to why we  will likely have a slow start to the season is because we have anomalously cool water across the  Main Development Region of the equatorial Atlantic and westwards into the Caribbean Sea.  This is indicative of further evidence of sinking air and suppression of warmth over these bodies of water, which typically contain warmer conducive for surface fuel for tropical systems by June.  So what does this mean for tropical cyclone development until those waters warm up? It really  points to the likelihood that we will be largely looking for homegrown systems that form near  our coastlines along old fronts with high pressure to their north giving them some “top spin”.  Just to be clear on this point, high pressure spins clockwise while low pressure spins counter-

clockwise. If we have strong high pressure north of a cold front that is near or over the coast,  then we can get low pressure(s) to spin up along that boundary. There is an old saying for this in  our profession, “Ridge over troubled waters” for the primary indicator when seeing the pattern  setting up.  

Source: Tropical Tidbits with edits by WeatherFlow Meteorologist Shea Gibson https://www.tropicaltidbits.com/analysis/ocean/ 

I also would like to discuss is the Saharan Air layer, or “SAL” for short. This is a very unique  natural/regular occurrence where strong winds over the Saharan Desert of Africa kick up lots of  sand and iron-rich and phosphorous-rich particles that are thrust up into the mid-levels of the  atmosphere. These particles are very light and due to buoyancy/lifting of the hot air, they are  suspended while traveling east over the Atlantic Ocean and slowly precipitate out over  thousands of miles. We call this the “Dry Dusty Tongue” of the Sahara and when the SAL  thickens during high wind events, this dust gets entrained into tropical waves that form just off  of Africa or even farther west in the Main Development region. It dries out the air an inhibits  convection and storming to aggregate around a surface circulation in its earliest stages and can  also plague a system that is trying to get its act together. Now this occurrence happens every  year regardless of what is happening in the Pacific, so I want to clarify that this is an additive and more of protective feature that tends to keep our hurricane activity down more than it  would be without it. In short, the SAL helps prevent many hurricanes from forming through the  summer, but relaxes a bit as we get into late summer and fall. Hence the “Cape Verde” season  when more storms form off the higher latitude of the equatorial Atlantic off the African coast  and make their routine runs to the west. 

Another key topic to touch on here as we head deeper into the season is our current hurricane  forecast accuracy. Honestly, it just keeps getting better and better over time and it is amazing to  be in such a rich era of data. The forecast cone of uncertainty has improved in both a reduction 

in cone width and a higher accuracy in its track to five days out. There is a new experimental  cone to be used this year that will express 90% of the forecast track possibilities instead of the  standard 67% forecast error, which means this accuracy is progged to take its next step forward  with even better results. Just in the last several years, the NHC has become very accurate within  50-60 miles at one to two days out, within 100 miles at day three and within 200 miles at days  four and five. In essence, the cone of uncertainty has shrunk significantly over time and shows continuous improvement. This has a lot to do with not only super-computing power /  numerical modeling becoming stronger, but also continued human interactive observation  techniques such as hurricane hunters, surface-based weather stations (we at WeatherFlow Tempest contribute to this!) and a better understanding of atmospheric steering patterns.

Speaking of model guidance, there has been a large surge in numerical prediction accuracy as  more data is being ingested into the physics and architecture of model ensembles, which host  dozens of solutions for each run to develop better mean solutions. Additionally, the statistical,  deterministic, probabilistic and dynamic modeling has become stronger as well as time has gone  

by. The recent introduction of AI tropical cyclone model guidance by various outfits such as the  AIGFS (AI Global Forecast System) in the US, EC-AIFS (Euro) and even Google are showing more  and more similarities in their runs, which is a good thing when models become aligned in the medium and short-term solutions. It should be very interesting to see how these models improve over time, but don’t forget that we still very much need human interaction for  guidance on these storms as intuitive tropics knowledge still supersedes the computing power  we have in many ways.

My final thoughts here will be given to a safety moment for all of us. Let’s always remember that it takes only one land-falling storm to change perspective on what we might perceive as a  quiet season ahead. Be sure to develop your evacuation plans and have your hurricane kits  updated just in case, especially if you live at the coast. It’s not a matter of IF, it’s WHEN.  

Stay safe and stay weather aware out there! Be sure to tune in to our WeatherFlow-Tempest  apps and products as we provide all kinds of quality key information for your needs in all things  weather!  

Sincerely, 

Weather-Flow Tempest Meteorologist Shea Gibson

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