{"id":1228,"date":"2026-10-29T14:32:58","date_gmt":"2026-10-29T18:32:58","guid":{"rendered":"https:\/\/climate.ncsu.edu\/learn\/?page_id=1228"},"modified":"2026-11-10T10:42:58","modified_gmt":"2026-11-10T15:42:58","slug":"science","status":"publish","type":"page","link":"https:\/\/climate.ncsu.edu\/learn\/hurricanes\/science\/","title":{"rendered":"Tropical Storm Science"},"content":{"rendered":"\n\n\n\n\n<div class=\"wp-block-group alignwide has-global-padding is-layout-constrained wp-block-group-is-layout-constrained\"><div class=\"is-text wp-block-ncst-buttons\">\n    \n<div class=\"is-style-secondary wp-block-ncst-button\">\n      <a\n        class=\"ncst-block__button-link btn\"\n        href=\"https:\/\/climate.ncsu.edu\/products\/weather\/hurricanes\/\"\n        data-ncst-lightbox=\"false\"\n                      >\n                  <span class=\"text\">Hurricanes Home<\/span><span class=\"arrow-indicator\"><svg class=\"wolficon wolficon-arrow-right-bold\" role=\"img\"  aria-hidden=\"true\">\n\t\t\t\n\t\t\t<use xlink:href=\"#wolficon-arrow-right-bold\">\n\t\t<\/svg><\/span>\n              <\/a>\n    <\/div>\n  \n\n<div class=\"is-style-default wp-block-ncst-button\">\n      <a\n        class=\"ncst-block__button-link btn\"\n        href=\"https:\/\/climate.ncsu.edu\/learn\/hurricanes\/science\/\"\n        data-ncst-lightbox=\"false\"\n                      >\n                  <span class=\"text\">Tropical Storm Science<\/span><span class=\"arrow-indicator\"><svg class=\"wolficon wolficon-arrow-right-bold\" role=\"img\"  aria-hidden=\"true\">\n\t\t\t\n\t\t\t<use xlink:href=\"#wolficon-arrow-right-bold\">\n\t\t<\/svg><\/span>\n              <\/a>\n    <\/div>\n  \n\n<div class=\"is-style-secondary wp-block-ncst-button\">\n      <a\n        class=\"ncst-block__button-link btn\"\n        href=\"https:\/\/climate.ncsu.edu\/learn\/hurricanes\/hazards\/\"\n        data-ncst-lightbox=\"false\"\n                      >\n                  <span class=\"text\">Hurricane Hazards<\/span><span class=\"arrow-indicator\"><svg class=\"wolficon wolficon-arrow-right-bold\" role=\"img\"  aria-hidden=\"true\">\n\t\t\t\n\t\t\t<use xlink:href=\"#wolficon-arrow-right-bold\">\n\t\t<\/svg><\/span>\n              <\/a>\n    <\/div>\n  \n\n<div class=\"is-style-secondary wp-block-ncst-button\">\n      <a\n        class=\"ncst-block__button-link btn\"\n        href=\"https:\/\/climate.ncsu.edu\/learn\/hurricanes\/climate-change\/\"\n        data-ncst-lightbox=\"false\"\n                      >\n                  <span class=\"text\">Climate Change and Hurricanes<\/span><span class=\"arrow-indicator\"><svg class=\"wolficon wolficon-arrow-right-bold\" role=\"img\"  aria-hidden=\"true\">\n\t\t\t\n\t\t\t<use xlink:href=\"#wolficon-arrow-right-bold\">\n\t\t<\/svg><\/span>\n              <\/a>\n    <\/div>\n  \n\n<div class=\"is-style-secondary wp-block-ncst-button\">\n      <a\n        class=\"ncst-block__button-link btn\"\n        href=\"https:\/\/climate.ncsu.edu\/learn\/hurricanes\/history\/\"\n        data-ncst-lightbox=\"false\"\n                      >\n                  <span class=\"text\">Notable Storms<\/span><span class=\"arrow-indicator\"><svg class=\"wolficon wolficon-arrow-right-bold\" role=\"img\"  aria-hidden=\"true\">\n\t\t\t\n\t\t\t<use xlink:href=\"#wolficon-arrow-right-bold\">\n\t\t<\/svg><\/span>\n              <\/a>\n    <\/div>\n  \n\n<div class=\"is-style-secondary wp-block-ncst-button\">\n      <a\n        class=\"ncst-block__button-link btn\"\n        href=\"https:\/\/climate.ncsu.edu\/products\/weather\/hurricanes\/nc-landfalls\/\"\n        data-ncst-lightbox=\"false\"\n                      >\n                  <span class=\"text\">Landfall in NC<\/span><span class=\"arrow-indicator\"><svg class=\"wolficon wolficon-arrow-right-bold\" role=\"img\"  aria-hidden=\"true\">\n\t\t\t\n\t\t\t<use xlink:href=\"#wolficon-arrow-right-bold\">\n\t\t<\/svg><\/span>\n              <\/a>\n    <\/div>\n  \n\n  <\/div>\n\n\n\n<p class=\"wp-block-paragraph\">Hurricanes have a beautiful symmetry, with rain bands spiraling around a cloud-free circular eye, that\u2019s a product of their step-by-step development and the scientific processes that drive it. From their formation as atmospheric seedlings to their strengthening at sea to their impacts on our state, science has a lot to say about how these storms work.<\/p>\n\n\n\n<h3 class=\"wp-block-heading\">Tropical Storm Life Cycle<\/h3>\n\n\n\n<p class=\"wp-block-paragraph\">Tropical storms are atmospheric phenomena that are fueled by the oceans. Throughout their lifetimes, these storms see a close interaction between air and water to help them develop, strengthen, and power their eventual impacts upon reaching land.<\/p>\n\n\n\n<h4 class=\"wp-block-heading\"><strong>Tropical Beginnings<\/strong><\/h4>\n\n\n\n<p class=\"wp-block-paragraph\">Each storm starts as an atmospheric disturbance, which can take a few different forms:<\/p>\n\n\n\n<ul class=\"wp-block-list\">\n<li>Sometimes, these storms can develop from a frontal boundary stalled over the warm water of the Gulf Stream off our east coast.<\/li>\n\n\n\n<li>Over the warm Caribbean or Gulf of Mexico, a cluster of thunderstorms can likewise become sufficiently organized to become a tropical system.<\/li>\n\n\n\n<li>Many long-lived storms that cross the Atlantic begin as weak-but-wet low-pressure systems called <a href=\"https:\/\/cpo.noaa.gov\/projections-of-tropical-cyclones-and-rainfall-in-the-african-sahel-could-be-improved-with-better-understanding-and-representation-of-african-easterly-waves-in-models\/\" target=\"_blank\" rel=\"noopener\"><em>African easterly waves<\/em><\/a> that form over the African continent before moving across the eastern Atlantic Ocean.<\/li>\n<\/ul>\n\n\n\n<p class=\"wp-block-paragraph\">No matter their atmospheric origins, these disturbances need warm water in the ocean beneath them to kickstart their tropical development. Typically, sea surface temperatures of at least 79\u00b0F (or 26\u00b0C) are needed for tropical storms to form. That water warms the air above it and evaporates to increase the humidity. That warm, moist air then rises in a process called <em>convection<\/em>, which causes thunderstorms to form and release the latent heat that <a href=\"http:\/\/www.atmo.arizona.edu\/students\/courselinks\/spring07\/atmo336s3\/lectures\/sec2\/hurricanes4.html\" target=\"_blank\" rel=\"noopener\">drives further development<\/a>.<\/p>\n\n\n\n<figure class=\"wp-block-image size-full is-resized\"><img loading=\"lazy\" decoding=\"async\" width=\"1024\" height=\"447\" src=\"https:\/\/climate.ncsu.edu\/learn\/wp-content\/uploads\/sites\/3\/2026\/10\/tc_structure-1024x447-1.png\" alt=\"A schematic of a typical tropical cyclone structure in the Northern Hemisphere\" class=\"wp-image-1236\" style=\"aspect-ratio:2.29082774049217;width:1024px;height:auto\" srcset=\"https:\/\/climate.ncsu.edu\/learn\/wp-content\/uploads\/sites\/3\/2026\/10\/tc_structure-1024x447-1.png 1024w, https:\/\/climate.ncsu.edu\/learn\/wp-content\/uploads\/sites\/3\/2026\/10\/tc_structure-1024x447-1-300x131.png 300w, https:\/\/climate.ncsu.edu\/learn\/wp-content\/uploads\/sites\/3\/2026\/10\/tc_structure-1024x447-1-768x335.png 768w\" sizes=\"auto, (max-width: 1024px) 100vw, 1024px\" \/><figcaption class=\"wp-element-caption\">The typical tropical cyclone structure, including warm rising air, or convection, around the eye and in outer rain bands. (<a href=\"https:\/\/commons.wikimedia.org\/wiki\/File:Hurricane-en.svg\" target=\"_blank\" rel=\"noopener\">Image<\/a> by Kelvinsong via Wikimedia Commons under <a href=\"https:\/\/creativecommons.org\/licenses\/by\/3.0\/\" target=\"_blank\" rel=\"noopener\">CC BY 3.0<\/a>)<\/figcaption><\/figure>\n\n\n\n<h4 class=\"wp-block-heading\"><strong>Storm Strengthening<\/strong><\/h4>\n\n\n\n<p class=\"wp-block-paragraph\">Once they start forming, these systems need a few other ingredients in place to help and not hinder their development:<\/p>\n\n\n\n<ul class=\"wp-block-list\">\n<li><strong>A moist atmosphere<\/strong> provides more fuel for clouds and thunderstorms, while dry air \u2013 including from <a href=\"https:\/\/www.wunderground.com\/hurricane\/articles\/saharan-dust-explainer\" target=\"_blank\" rel=\"noopener\">Saharan dust<\/a> blown across the main development region of the Atlantic \u2013 can sap the moisture within a storm.<\/li>\n\n\n\n<li><a href=\"https:\/\/www.wunderground.com\/hurricane\/articles\/wind-shear-explainer\"><strong>Wind shear<\/strong><\/a>, or the change in winds with increasing height in the atmosphere, can rip apart the clouds and thunderstorms in and around the developing eye of a tropical storm. Low vertical wind shear, particularly with weaker upper-level wind speeds, gives storms more breathing room for upward development.<\/li>\n\n\n\n<li><strong>An unstable atmosphere<\/strong>, characterized by warmer air near the surface and cooler air aloft, means that warm and moist air can rise in strong updrafts that help further grow the thunderstorms at the heart of these tropical systems.<\/li>\n<\/ul>\n\n\n\n<p class=\"wp-block-paragraph\">If these ingredients come together, the once-disorganized disturbance will coalesce around a thunderstorm-laden core, with outer rain bands rotating around a low-pressure center of circulation.<\/p>\n\n\n\n<figure class=\"wp-block-image size-full is-resized\"><img loading=\"lazy\" decoding=\"async\" width=\"930\" height=\"523\" src=\"https:\/\/climate.ncsu.edu\/learn\/wp-content\/uploads\/sites\/3\/2026\/10\/sat_Bertha_2020.jpg\" alt=\"Satellite imagery of Tropical Storm Bertha at its landfall in South Carolina in 2020\" class=\"wp-image-1235\" style=\"aspect-ratio:1.7782026768642447;width:930px;height:auto\" srcset=\"https:\/\/climate.ncsu.edu\/learn\/wp-content\/uploads\/sites\/3\/2026\/10\/sat_Bertha_2020.jpg 930w, https:\/\/climate.ncsu.edu\/learn\/wp-content\/uploads\/sites\/3\/2026\/10\/sat_Bertha_2020-300x169.jpg 300w, https:\/\/climate.ncsu.edu\/learn\/wp-content\/uploads\/sites\/3\/2026\/10\/sat_Bertha_2020-768x432.jpg 768w, https:\/\/climate.ncsu.edu\/learn\/wp-content\/uploads\/sites\/3\/2026\/10\/sat_Bertha_2020-750x422.jpg 750w\" sizes=\"auto, (max-width: 930px) 100vw, 930px\" \/><figcaption class=\"wp-element-caption\">Infrared satellite imagery showed Bertha as a disorganized and minimal tropical storm at its landfall in South Carolina on May 27, 2020. (Image by NOAA\/GOES via <a href=\"https:\/\/www.wunderground.com\/cat6\/that-was-fast-tropical-storm-bertha-develops-and-makes-landfall-over-south-carolina\" target=\"_blank\" rel=\"noopener\">Weather Underground<\/a>)<\/figcaption><\/figure>\n\n\n\n<h4 class=\"wp-block-heading\"><strong>Classification<\/strong><\/h4>\n\n\n\n<p class=\"wp-block-paragraph\">As tropical systems become better organized, they can be classified in one of the following ways based on the maximum sustained winds, typically located near the center of circulation or in the eyewall of stronger storms.<\/p>\n\n\n\n<ul class=\"wp-block-list\">\n<li>The pressure difference between the heart of these storms and their surrounding environment powers winds that spiral toward the center. Once the maximum sustained winds reach 38 miles per hour, a system is classified as a <strong>tropical depression<\/strong>.<\/li>\n\n\n\n<li>With winds of at least 39 miles per hour, it becomes a <strong>tropical storm<\/strong> and is given a name from a <a href=\"https:\/\/www.nhc.noaa.gov\/aboutnames.shtml\" target=\"_blank\" rel=\"noopener\">regional list<\/a> curated by the World Meteorological Organization. <a href=\"https:\/\/www.nhc.noaa.gov\/aboutnames_history.shtml\" target=\"_blank\" rel=\"noopener\">Storm naming<\/a> began within the US military to help internal communications about these systems, and it became a public communications tool during the 1950s.<\/li>\n\n\n\n<li>Once a storm\u2019s sustained winds reach 74 miles per hour or greater, it becomes a <strong>hurricane<\/strong> in the north Atlantic basin, with further categorization based on the <a href=\"https:\/\/www.nhc.noaa.gov\/aboutsshws.php\" target=\"_blank\" rel=\"noopener\">Saffir-Simpson scale<\/a>. Hurricanes often feature a classic look with a cloud-free eye ringed by an intense, stormy eyewall and flanked by outer bands. This structure ultimately helps these storms keep their strength, as air circulates from their warm core to the cool upper levels of the atmosphere on their fringes.<\/li>\n<\/ul>\n\n\n\n<figure class=\"wp-block-image size-full is-resized\"><img loading=\"lazy\" decoding=\"async\" width=\"1024\" height=\"575\" src=\"https:\/\/climate.ncsu.edu\/learn\/wp-content\/uploads\/sites\/3\/2026\/10\/Isabel_satellite_Cat5.jpg\" alt=\"Satellite imagery of Hurricane Isabel near its maximum intensity on September 14, 2003\" class=\"wp-image-1234\" style=\"aspect-ratio:1.7808695652173914;width:1024px;height:auto\" srcset=\"https:\/\/climate.ncsu.edu\/learn\/wp-content\/uploads\/sites\/3\/2026\/10\/Isabel_satellite_Cat5.jpg 1024w, https:\/\/climate.ncsu.edu\/learn\/wp-content\/uploads\/sites\/3\/2026\/10\/Isabel_satellite_Cat5-300x168.jpg 300w, https:\/\/climate.ncsu.edu\/learn\/wp-content\/uploads\/sites\/3\/2026\/10\/Isabel_satellite_Cat5-768x431.jpg 768w, https:\/\/climate.ncsu.edu\/learn\/wp-content\/uploads\/sites\/3\/2026\/10\/Isabel_satellite_Cat5-750x422.jpg 750w\" sizes=\"auto, (max-width: 1024px) 100vw, 1024px\" \/><figcaption class=\"wp-element-caption\">Hurricane Isabel near its maximum, Category-5 strength, with a broad eye more than 45 miles wide. (Image by NOAA)<\/figcaption><\/figure>\n\n\n\n<h4 class=\"wp-block-heading\"><strong>Late in Life<\/strong><\/h4>\n\n\n\n<p class=\"wp-block-paragraph\">While a hurricane can remain active for days or even weeks, they all eventually come to an end through one or more of the following ways:<\/p>\n\n\n\n<ul class=\"wp-block-list\">\n<li>The tropical Atlantic offers a 3,000-mile runway of warm ocean water to fuel developing hurricanes, but on the western edge of the ocean are the landmasses of north and central America. When storms move over this land, they\u2019re cut off from their warm water fuel and their winds are weakened by the frictional effects of the rough land surface. This stops their development and causes them to weaken.<\/li>\n\n\n\n<li>Due to the earth\u2019s rotation, hurricanes naturally curve toward the poles during their lifetimes \u2013 a result of the <a href=\"https:\/\/education.nationalgeographic.org\/resource\/coriolis-effect-1\/\" target=\"_blank\" rel=\"noopener\">Coriolis effect<\/a> that causes moving air to deflect to the right in the Northern Hemisphere. As storms move poleward, they eventually move over either land or colder water, which ends their tropical lifespans. In some cases, they can then become <a href=\"https:\/\/www.nps.gov\/articles\/extratropical-storms.htm\" target=\"_blank\" rel=\"noopener\"><em>extratropical cyclones<\/em><\/a>, which can still pack some high winds and other intense impacts, but that become frontal in nature as the warm-natured storms venturing into colder environments.<\/li>\n\n\n\n<li>Hurricanes aren\u2019t the only weather systems in the atmosphere; cold fronts and other low-pressure areas are always circulating as well, and when these systems meet, they can interact \u2013 sometimes enhancing a tropical storm\u2019s impacts, such as feeding it more moisture as during <a href=\"https:\/\/climate.ncsu.edu\/blog\/2020\/11\/rapid-reaction-eta-aided-rain-event-drenches-nc\/\" target=\"_blank\" rel=\"noopener\">Tropical Storm Eta<\/a> in 2020, but eventually eroding a tropical storm\u2019s structure and causing it to lose its tropical characteristics.<\/li>\n<\/ul>\n\n\n\n<h3 class=\"wp-block-heading\">Seasonality<\/h3>\n\n\n\n<p class=\"wp-block-paragraph\">The Atlantic hurricane season runs from June through November, but each of those six months has its own unique characteristics in terms of where tropical storms tend to form:<\/p>\n\n\n\n<ul class=\"wp-block-list\">\n<li><strong>Early in the season<\/strong> \u2014 and sometimes, even in April or May, before hurricane season officially begins \u2013 storms are most likely to form where the ocean water is warmest, either in the Gulf of Mexico or over the Gulf Stream current that runs along our east coast.<\/li>\n\n\n\n<li>By <strong>mid-summer<\/strong>, as the rest of the Atlantic\u2019s main development region warms up, storms typically begin developing off the coast of Africa by August, with a \u201cconveyor belt\u201d of disturbances and storms often setting up by the peak of the season in September.<\/li>\n\n\n\n<li>By <strong>late-season<\/strong> in the <strong>fall<\/strong>, the still-warm parts of the western Atlantic become the favored regions for any late-season storms, and as the upper-level winds such as the jet streams strengthen, they sometimes push storms from west to east rather than their more common east-to-west trajectories.<\/li>\n<\/ul>\n\n\n\n<div class=\"wp-block-columns is-layout-flex wp-container-core-columns-is-layout-8f761849 wp-block-columns-is-layout-flex\">\n<div class=\"wp-block-column is-layout-flow wp-block-column-is-layout-flow\">\n<figure class=\"wp-block-image size-full is-resized\"><img loading=\"lazy\" decoding=\"async\" width=\"768\" height=\"593\" src=\"https:\/\/climate.ncsu.edu\/learn\/wp-content\/uploads\/sites\/3\/2026\/10\/atl_climo_ns_jun-768x593-1.jpg\" alt=\"A map of historical Atlantic tropical storm occurrence during the month of June\" class=\"wp-image-1233\" style=\"aspect-ratio:1.2945638432364097;width:1024px;height:auto\" srcset=\"https:\/\/climate.ncsu.edu\/learn\/wp-content\/uploads\/sites\/3\/2026\/10\/atl_climo_ns_jun-768x593-1.jpg 768w, https:\/\/climate.ncsu.edu\/learn\/wp-content\/uploads\/sites\/3\/2026\/10\/atl_climo_ns_jun-768x593-1-300x232.jpg 300w\" sizes=\"auto, (max-width: 768px) 100vw, 768px\" \/><\/figure>\n<\/div>\n\n\n\n<div class=\"wp-block-column is-layout-flow wp-block-column-is-layout-flow\">\n<figure class=\"wp-block-image size-full is-resized\"><img loading=\"lazy\" decoding=\"async\" width=\"768\" height=\"593\" src=\"https:\/\/climate.ncsu.edu\/learn\/wp-content\/uploads\/sites\/3\/2026\/10\/atl_climo_ns_sep-768x593-1.jpg\" alt=\"A map of historical Atlantic tropical storm occurrence during the month of September\" class=\"wp-image-1232\" style=\"aspect-ratio:1.2945638432364097;width:1024px;height:auto\" srcset=\"https:\/\/climate.ncsu.edu\/learn\/wp-content\/uploads\/sites\/3\/2026\/10\/atl_climo_ns_sep-768x593-1.jpg 768w, https:\/\/climate.ncsu.edu\/learn\/wp-content\/uploads\/sites\/3\/2026\/10\/atl_climo_ns_sep-768x593-1-300x232.jpg 300w\" sizes=\"auto, (max-width: 768px) 100vw, 768px\" \/><\/figure>\n<\/div>\n\n\n\n<div class=\"wp-block-column is-layout-flow wp-block-column-is-layout-flow\">\n<figure class=\"wp-block-image size-full is-resized\"><img loading=\"lazy\" decoding=\"async\" width=\"768\" height=\"593\" src=\"https:\/\/climate.ncsu.edu\/learn\/wp-content\/uploads\/sites\/3\/2026\/10\/atl_climo_ns_nov-768x593-1.jpg\" alt=\"A map of historical Atlantic tropical storm occurrence during the month of November\" class=\"wp-image-1231\" style=\"aspect-ratio:1.2945638432364097;width:1024px;height:auto\" srcset=\"https:\/\/climate.ncsu.edu\/learn\/wp-content\/uploads\/sites\/3\/2026\/10\/atl_climo_ns_nov-768x593-1.jpg 768w, https:\/\/climate.ncsu.edu\/learn\/wp-content\/uploads\/sites\/3\/2026\/10\/atl_climo_ns_nov-768x593-1-300x232.jpg 300w\" sizes=\"auto, (max-width: 768px) 100vw, 768px\" \/><\/figure>\n<\/div>\n<\/div>\n\n\n\n<p class=\"wp-block-paragraph\"><em>Historical occurrence areas for Atlantic named storms in <strong>June<\/strong> (left), <strong>September<\/strong> (middle), and <strong>November<\/strong> (right). Maps from <a href=\"https:\/\/www.nhc.noaa.gov\/climo\/#ori\" target=\"_blank\" rel=\"noopener\">NHC<\/a>.<\/em><\/p>\n\n\n\n<h3 class=\"wp-block-heading\">North Carolina\u2019s Climatology<\/h3>\n\n\n\n<p class=\"wp-block-paragraph\">Our state\u2019s unique geography adds to our susceptibility to tropical storms. <a href=\"https:\/\/climate.ncsu.edu\/blog\/2022\/07\/our-curious-coast-the-ocean-and-coastline\/\" target=\"_blank\" rel=\"noopener\">Our coastline<\/a> juts out several hundred miles compared to the land to our south, with a warm offshore ocean current called the <em>Gulf Stream<\/em> acting as an alleyway where strong storms can form and move. In addition, storms making landfall in the Gulf of Mexico can move northward, with their remnants affecting parts of western North Carolina.<\/p>\n\n\n\n<p class=\"wp-block-paragraph\">Past analysis at our office identified historical tropical storms that affected North Carolina \u2013 including landfalling storms, remnant systems that moved over us, and storms that brought rain or other impacts to parts of the state \u2013 between 1851 and 2019.<\/p>\n\n\n\n<p class=\"wp-block-paragraph\">We found a total of 387 storms that either made landfall or passed within 150 miles of our state, which was <a href=\"https:\/\/climate.ncsu.edu\/learn\/wp-content\/uploads\/sites\/3\/2026\/11\/NC_TCstats_1851-2019.png\" target=\"_blank\" rel=\"noopener\">19.3% of all Atlantic tropical storms<\/a> during that 169-year period. That means <strong>2.3 storms per year affect North Carolina, on average<\/strong>, with one storm every two years making <a href=\"https:\/\/climate.ncsu.edu\/products\/weather\/hurricanes\/nc-landfalls\/\" target=\"_blank\" rel=\"noopener\">direct landfall<\/a>.<\/p>\n\n\n\n<figure class=\"wp-block-image size-full is-resized\"><img loading=\"lazy\" decoding=\"async\" width=\"1024\" height=\"591\" src=\"https:\/\/climate.ncsu.edu\/learn\/wp-content\/uploads\/sites\/3\/2026\/10\/Dorian_sat_offshore-1024x591-1.jpg\" alt=\"A satellite image of Hurricane Dorian off the coast of North Carolina in 2019\" class=\"wp-image-1230\" style=\"aspect-ratio:1.7326565143824026;width:1024px;height:auto\" srcset=\"https:\/\/climate.ncsu.edu\/learn\/wp-content\/uploads\/sites\/3\/2026\/10\/Dorian_sat_offshore-1024x591-1.jpg 1024w, https:\/\/climate.ncsu.edu\/learn\/wp-content\/uploads\/sites\/3\/2026\/10\/Dorian_sat_offshore-1024x591-1-300x173.jpg 300w, https:\/\/climate.ncsu.edu\/learn\/wp-content\/uploads\/sites\/3\/2026\/10\/Dorian_sat_offshore-1024x591-1-768x443.jpg 768w\" sizes=\"auto, (max-width: 1024px) 100vw, 1024px\" \/><figcaption class=\"wp-element-caption\">North Carolina\u2019s eastward-extending coastline makes it an easy target for storms such as Hurricane Dorian. (Image by NOAA\/GOES)<\/figcaption><\/figure>\n\n\n\n<p class=\"wp-block-paragraph\">As with the overall Atlantic basin, the peak of the season between early September and mid-October is our most active period. However, we also see a secondary increase in activity in June and July associated with early-season storms forming over the warm water just off our coastline.<\/p>\n\n\n\n<figure class=\"wp-block-image size-large\"><img loading=\"lazy\" decoding=\"async\" width=\"1024\" height=\"716\" src=\"https:\/\/climate.ncsu.edu\/learn\/wp-content\/uploads\/sites\/3\/2026\/10\/NC_weekly_TC_climo-1024x716.png\" alt=\"Chart of weekly tropical cyclone activity for NC\" class=\"wp-image-1229\" srcset=\"https:\/\/climate.ncsu.edu\/learn\/wp-content\/uploads\/sites\/3\/2026\/10\/NC_weekly_TC_climo-1024x716.png 1024w, https:\/\/climate.ncsu.edu\/learn\/wp-content\/uploads\/sites\/3\/2026\/10\/NC_weekly_TC_climo-300x210.png 300w, https:\/\/climate.ncsu.edu\/learn\/wp-content\/uploads\/sites\/3\/2026\/10\/NC_weekly_TC_climo-768x537.png 768w, https:\/\/climate.ncsu.edu\/learn\/wp-content\/uploads\/sites\/3\/2026\/10\/NC_weekly_TC_climo.png 1200w\" sizes=\"auto, (max-width: 1024px) 100vw, 1024px\" \/><\/figure>\n\n\n\n<p class=\"wp-block-paragraph\">An overall active season in the Atlantic is no guarantee of an active season in North Carolina. If large-scale atmospheric patterns such as the <a href=\"https:\/\/svs.gsfc.nasa.gov\/10069\" target=\"_blank\" rel=\"noopener\">Bermuda high pressure system<\/a> are parked over us for much of the hurricane season, then those features can act as a roadblock and steer storms away from us. This was the case in <a href=\"https:\/\/products.climate.ncsu.edu\/weather\/hurricanes_database\/?search=year&amp;yr=2023\" target=\"_blank\" rel=\"noopener\">2023<\/a>, when 20 total storms formed in the Atlantic basin but only 3 of them made landfall in the mainland US, including just one \u2013 <a href=\"https:\/\/climate.ncsu.edu\/blog\/2023\/09\/rapid-reaction-surprisingly-strong-ophelia-surges-in\/\" target=\"_blank\" rel=\"noopener\">Tropical Storm Ophelia<\/a> \u2013 in North Carolina.<\/p>\n\n\n\n<p class=\"wp-block-paragraph\">On the other hand, a quiet season with few named storms can still be an impactful and memorable one if even one of those storms affects us locally. For example, 1960 featured only <a href=\"https:\/\/products.climate.ncsu.edu\/weather\/hurricanes_database\/?search=year&amp;yr=1960\" target=\"_blank\" rel=\"noopener\">six named storms<\/a>, but among them, <a href=\"https:\/\/www.weather.gov\/ilm\/top_20_storms#3\" target=\"_blank\" rel=\"noopener\">Hurricane Donna<\/a> impacted Florida as a Category-4 and North Carolina as a still-damaging Category-2 hurricane.<\/p>\n<\/div>\n","protected":false},"excerpt":{"rendered":"<p>Hurricanes have a beautiful symmetry, with rain bands spiraling around a cloud-free circular eye, that\u2019s a product of their step-by-step development and the scientific processes that drive it. From their formation as atmospheric seedlings to their strengthening at sea to their impacts on our state, science has a lot to say about how these storms&hellip;<\/p>\n","protected":false},"author":2,"featured_media":0,"parent":33,"menu_order":0,"comment_status":"closed","ping_status":"closed","template":"","meta":{"_acf_changed":false,"source":"","ncst_custom_author":"","ncst_show_custom_author":false,"ncst_dynamicHeaderBlockName":"ncst\/default-header","ncst_dynamicHeaderData":"{}","ncst_content_audit_freq":"","ncst_content_audit_date":"","ncst_content_audit_display":false,"ncst_backToTopFlag":"","footnotes":""},"coauthors":[2],"class_list":["post-1228","page","type-page","status-publish","hentry"],"acf":[],"_links":{"self":[{"href":"https:\/\/climate.ncsu.edu\/learn\/wp-json\/wp\/v2\/pages\/1228","targetHints":{"allow":["GET"]}}],"collection":[{"href":"https:\/\/climate.ncsu.edu\/learn\/wp-json\/wp\/v2\/pages"}],"about":[{"href":"https:\/\/climate.ncsu.edu\/learn\/wp-json\/wp\/v2\/types\/page"}],"author":[{"embeddable":true,"href":"https:\/\/climate.ncsu.edu\/learn\/wp-json\/wp\/v2\/users\/2"}],"replies":[{"embeddable":true,"href":"https:\/\/climate.ncsu.edu\/learn\/wp-json\/wp\/v2\/comments?post=1228"}],"version-history":[{"count":7,"href":"https:\/\/climate.ncsu.edu\/learn\/wp-json\/wp\/v2\/pages\/1228\/revisions"}],"predecessor-version":[{"id":1319,"href":"https:\/\/climate.ncsu.edu\/learn\/wp-json\/wp\/v2\/pages\/1228\/revisions\/1319"}],"up":[{"embeddable":true,"href":"https:\/\/climate.ncsu.edu\/learn\/wp-json\/wp\/v2\/pages\/33"}],"wp:attachment":[{"href":"https:\/\/climate.ncsu.edu\/learn\/wp-json\/wp\/v2\/media?parent=1228"}],"wp:term":[{"taxonomy":"author","embeddable":true,"href":"https:\/\/climate.ncsu.edu\/learn\/wp-json\/wp\/v2\/coauthors?post=1228"}],"curies":[{"name":"wp","href":"https:\/\/api.w.org\/{rel}","templated":true}]}}