The Great Hurricanes of North Carolina
By John Hairr
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About this ebook
John Hairr
John Hairr is an award winning writer and historian who has written extensively about the history and lore of the southeastern United States and the Caribbean region. His writings have covered a wide range of topics, including wild rivers, shipwrecks and extinct wildlife. A member of the Outdoor Writers Association of America, his work has appeared in numerous publications including Mercator's World, South Carolina Wildlife and Fortean Times.
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The Great Hurricanes of North Carolina - John Hairr
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INTRODUCTION
Hurricanes have long been a fact of life in the Carolinas. With its lengthy, exposed coastline jutting into the Atlantic Ocean and reaching out nearly to the Gulf Stream, there is little wonder that these tempests have visited the land since before there was a North or South Carolina. Hurricanes have literally shaped the land along our coast, and in a sense, the people as well.
This book discusses the most fearsome and violent hurricanes that have made landfall along the North Carolina coast. All hurricanes have the potential to be destructive, but throughout the years several hurricanes that have visited the state were notable for a variety of factors, including high winds, massive floods or the large number of fatalities they left in their wakes. In a land that is frequently visited by tropical storms, each generation seems to have a benchmark storm against which all others are measured. This book takes a look at all of these storms, and investigates the state’s most powerful and memorable hurricanes.
Storm debris from Hurricane Hazel litters the mainland near Lockwood’s Folly Inlet in Brunswick County. Photo courtesy Wilmington District, U.S. Army Corps of Engineers.
A hurricane is a tropical cyclone with maximum sustained winds of seventy-four miles per hour or greater. Tropical cyclones are systems of large, rotating thunderstorms that form over warm, tropical water. Due to the effects of the earth’s rotation, these storms rotate in a counterclockwise fashion in the Northern Hemisphere, and rotate clockwise in the Southern Hemisphere. They are found in all areas of the tropical regions of the world. These tropical cyclones are called hurricanes in the North Atlantic once they exceed the seventy-four-mile-per-hour threshold.
The word hurricane
has its origins in the names given to the storm gods by various tribes of Native Americans inhabiting the islands and mainland surrounding the Caribbean. It is certain that the Native Americans who inhabited the land we now call North Carolina experienced the high winds and heavy rains of these storms. Unfortunately, they left no written accounts of their experiences.
The Calypso was battered by the high winds and heavy seas it encountered in a fierce hurricane that struck the North Carolina coast in August of 1837. Captain Gilbert Wilkinson, master of the Calypso, managed to bring his severely damaged vessel into port inside the Cape Fear River. He afterward observed: We were kindly received by the good people at Smithville and Wilmington who complained bitterly of the late storm, for many of their houses were unroofed, and trees blown down.
When the Europeans first attempted to found settlements along the coast, they quickly learned about these storms. Sir Francis Drake, who had traveled the seas of the globe in quest of glory and plunderage, nearly lost his fleet on the Outer Banks during an encounter with a hurricane in June of 1586. His ships were anchored just off the banks while he checked on the progress of Sir Walter Raleigh’s colonists on Roanoke Island. The hurricane lasted three days, scattering Drake’s fleet and nearly destroying many of his ships.
As time passed and settlers learned more about their new homeland, they experienced these storms on such a regular basis that they became accustomed to them. Eventually they began calling them equinoctial storms, as the storms normally hit in the weeks around the period of the fall equinox, which in the Northern Hemisphere occurs in late September.
Thanks to four hundred years of observations and advances in technology, we now know that hurricanes can strike at any time between June and November. The peak of hurricane season in the Carolinas is in the month of September. Several early storms have been chronicled in June, the earliest striking on June 2, 1825. Only a handful of late-season storms have hit in November and December. The latest recorded storm moved out of the Caribbean and struck the North Carolina coast on December 2, 1925.
In 1858, Dr. David Ramsey, an eminent authority on the early history of South Carolina, wrote the following observations about these storms in the early days of European settlement in the Carolinas:
The autumnal equinox seldom passes in the vicinity of the torrid zone without some conflict of the elements more or less dangerous. In the 138 years which have taken place since the settlement of Carolina, several minor storms have passed over without exciting any permanent public attention. But four having done extensive mischief, are particularly remembered, and have been called hurricanes, an appellation usually given to those convulsive storms in the West India Islands in which the fields of sugar canes are destroyed, and the canes torn up and hurried away in confusion.
Ramsey wrote that the four hurricanes that did extensive mischief
along the Carolina coast were the ones occurring in 1700, 1728, 1752 and 1804. All were particularly bad storms, but the one that occurred on September 15, 1752, was perhaps the most severe. It was the first of two powerful hurricanes to strike the Carolina coast in as many weeks. Charles Town was inundated, ships were wrecked and many people lost their lives. Two weeks later, another violent hurricane struck South Carolina, though it was not as destructive in Charles Town as the first storm had been. This killer storm made landfall somewhere between Winyah Bay and Cape Fear before heading north and ravaging the North Carolina coast. This was the storm that destroyed the town of Johnston, the former county seat of Onslow County.
There were other notable hurricanes that struck back in the days when North Carolina was still a colony of Great Britain. One occurred in September 1761 when waters breached the Haulover,
which was a sandbank separating the Atlantic from the Cape Fear River. The resulting channel was found to be eighteen feet deep, but it filled in somewhat before stabilizing at about nine feet deep. The channel, dubbed New Inlet, remained open for over a century until it was closed by a rock dam constructed by the United States Army Corps of Engineers.
On September 7, 1769, a powerful hurricane that landed somewhere between Cape Fear and Cape Lookout flattened the Brunswick County courthouse and nearly flattened the town of New Bern. At Brunswick Town, Governor William Tryon wrote:
In short, my Lord, the inhabitants never knew such a storm; every herbage in the gardens had their leaves cut off. This hurricane is attributed to the effects of a blazing planet or star that was seen both from Newbern and here rising in the east for several nights between the 26th and 31st of August, its stream very long & stretched upwards towards the So West.
We know quite a bit more today about the origin and nature of hurricanes than Governor Tryon did back in 1769, or at least we think we do. Tropical cyclones frequently begin as an organized area of thunderstorm activity that holds together for twenty-four hours. As a tropical disturbance gets better organized, rotation becomes more pronounced, and once an area of closed circulation forms, it becomes a tropical depression. As the tropical depression intensifies and the sustained winds increase to thirty-nine miles per hour, the depression becomes a tropical storm. The system becomes a full-blown hurricane as winds exceed seventy-four miles per hour.
As the winds at the center of the storm increase to hurricane force, the ring of intense storms begins to form around the center of circulation. This wall of thunderstorms is called the eyewall,
and it is the portion of a hurricane that contains the strongest winds. At the center of a tropical cyclone, the area at the very center of the vortex is known as the eye, and it becomes more pronounced as the thunderstorms intensify. The eye of a storm is normally an area of light winds, clear to partly cloudy skies and no rain. The size of a hurricane’s eye varies from storm to storm, ranging in size from just a few miles across to over fifty miles across. In addition, the eye of any given storm will expand and contract as the hurricane interacts with other forces.
Conditions inside the eye of a hurricane can be quite bizarre, with low pressure affecting the ears. Reuben Frost, weather bureau chief for the National Weather Service at Wilmington, North Carolina, interviewed many people who experienced Hurricane Hazel in 1954. He collected some interesting observations about conditions as the eye of the storm passed over southeastern North Carolina, and he wrote the following valuable observations about the eye of the storm at Calabash:
Local people on the North Carolina coast use the Old English pronunciation of kam
for calm. People at Calabash stated the sudden kamming
of the wind and low pressure affected their ears, and there was a spooky, eerie feeling or sensation. One local lady said the kam
spell gave her the creeps.
After a few minutes she saw a very black and ugly bank of clouds approaching from the southwest. There was an awful roaring noise that scared her more than ever. In just a matter of seconds the kam
was over and the awful wind began