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Early spring often brings the most violent weather to the nation’s midsection of the entire year. High in the atmosphere, up where the jet stream is, temperatures can still be almost as cold as they are in mid-winter, yet down on the ground temperatures can soar to at times close to summer-time levels. The extreme temperature contrast, that occurs at no other time of the year, combined with turning winds from the surface up into higher levels of the air leads to the formation of severe thunderstorms and multiple tornados. On March 18, 1925 perhaps the greatest severe weather event in the last two centuries was brewing. By the time the day was over what would be known as the Tristate tornado produced the single most devastating tornado ever. The tornado began near Ellington, Missouri and averaged 62 mph in forward speed as it moved northeastward. The tornado was 1 mile wide and was on the ground for 219 miles the longest continuous tornado path ever observed. 85 farms were destroyed near Owensville, Indiana, and the entire town of Griffin, Indiana, was totally destroyed. A total of 695 deaths were reported with 2,027 injured there alone from that single tornado alone. There was $16.5 million worth of damage or almost a quarter of a billion in 2021 dollars. 11 other tornadoes the same day killed 50 more elsewhere, including 33 at a school in Desoto, IL.
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On March 4 and into March 5, 1776 American forces moved the guns onto Dorchester Heights that overlooked Boston from the south. It gave the Colonials a commanding position that the British could not counter. But British General William Howe wanted to give it a go anyway, he gathered some of his force of 11,000 troops onto ships to cross Boston harbor and attack the gun placements before they could be firmly established. Just as the troops had been loaded into the ships a huge storm hit and caused them to turn back. It gave the Americans time to firm up the guns and their advantage was established. The weather turned the tide. The British soon abandoned Boston, never to return during the rest of the Revolution. They evacuated on March 17, 1776, a day still celebrated in Boston.
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On March 16, 1843 one the first winter storms to be documented swept out of the Gulf of Mexico and impacted most of the eastern part of the nation.
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During the drought of the 1930s, un-anchored soil turned to dust, which the prevailing winds blew away in huge clouds that sometimes blackened the sky. These choking billows of dust were named "black blizzards". On March 15, 1935 one of the worst of these black blizzards, stuck Amarillo, Texas with Suffocating dust; 6 people died, many livestock starved or suffocated. Dust lay 6 feet deep in places.
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The term blizzard has found a significant spot in our language. A blizzard is officially defined as a storm with "considerable falling or blowing snow" and winds in excess of 35 mph with visibilities of less than 1/4 mile for at least 3 hours. The term has been applied to many snowstorms in American history, most notably the Blizzard of ’88. The term has also been used for snow events that did not meet the criteria – but where big snowstorms none the less. But the term wasn’t even invented until March 14 1870. The Editor of the Dakota Republican of Vermillion South Dakota described the storm: "A violent snowstorm, driven by a heavy NW wind, and continued three whole days and nights. The weather was intensely cold and the heavy fall, flying before a furious wind - blowing as only the prairie winds can blow - rendered traveling exceedingly uncomfortable and dangerous, if not almost impossible." This storm referred to as a blizzard. A baseball team was named after it: The "Northern Blizzards", of Estherville Iowa. The manager said that "We confess to a certain liking for it, because it's at once startling, curious and positively suggestive of the furious and all victorious tempests which are experienced in this northwestern clime."
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Records show that early settlers to what would become the Mid-Atlantic and New England states report of huge snowstorms dating back to the 1600s. Native American tales tell of deep snow and powerful winds from well before that time in the region. But modern city life and dense population was not yet established. By the 1880s though the population of Northeast cites had skyrocketed. In Philadelphia the population went from 120,000 in 1850 to 850,000 in 1880. NYC from 700,000 in 1850 to almost 2 million in 1880. With all those people packed into now modern rising cities and dependent on public services to allow people to get around and supply lines for basics like food major snow storms had a profound impact. In the decades prior to 1888 there had been no large snowstorm to impact the cities in the area. That all changed starting on March 11, 1888 and reached it’s height on March 13. In what would go down in history as the fabled Blizzard of ’88. The storm was slow to organize on the mid-Atlantic coast with 10” in Philadelphia, then it strengthened rapidly turning into a bomb cyclone. When the snow stopped flying the damage was done; more than 20” in New York 45” in Albany and New Haven Conn. New York City ground to a near halt in the face of massive snow drifts and powerful winds from the storm. Wind gusts were recorded at 85 miles per hour in New York City. Along with heavy snow, there was a complete whiteout in the city. Despite drifts that reached the second story of some buildings, many city residents trudged out to New York’s elevated trains to go to work, only to find many of them blocked by snow drifts and unable to move. Up to 15,000 people were stranded on the elevated trains. In addition to the elevated trains; telegraph lines, water mains and gas lines were also located above ground making them prone to freezing, which they did because record cold accompanied the storm, temperatures plunged into the teens as far south as North Carolina. At the time, approximately one in every four Americans lived in the area between Washington DC and Boston, more than 400 people perished in the storm. Even though it happened more than 130 years ago it is still the benchmark that all other storms are measured by in the region.
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The winter of 1989-1990 in the eastern 2/3rds of the nation had been brutal. November 1989 started mild in the western part of the nation, and a bit cooler in the East it was nothing out of the ordinary. The weather, however changed dramatically in late November. It turned very cold with frequent snowstorms in the central states and the east. In the Midwest temperatures averaged, in some places more than 15 degrees below normal, and it ranked as one of the 5 coldest Decembers on record, and the fierce winter was just getting started. At the end of December, just a day before Christmas one of the greatest coastal snowstorms every recorded struck South and North Carolina. By Christmas morning 1989 snow reached almost 4” in depth in Charleston, SC, 15” in Wilmington NC and more than a foot all the way out on Cape Hatteras, NC. Snow covered the ground as far south as Tampa and Daytona Beach. In January and February of 1990 temperatures began to moderate somewhat – but it remained cold and snowy in many places in the East. In mid-March winter broke and it did so by completely flipping the script. Warm air started to build across the Plains states and by March 10th the jet stream, that had dropped far south in the United States and brought cold air with it had retreated quickly northward into Canada. That allowed the warm air out west to pour into the East. March 12 , 1990 saw unheard of record high temperatures. The mercury reached 90 in Raleigh, NC, 87 in Norfolk, Va. 86 on the beaches of Atlantic City. And amazing 95 in Baltimore Md, breaking a record that had stood for 100 years. Meanwhile cool air still held out over New England and Long Island. While readings in northern New Jersey soared into the upper 80s, central Long Island was chilly. LaGuardia Airport, a mere 60 miles away in New York City reached no higher than 47. But the winter was clearly on the run on March 12, 1990 and no more artic air reached into the Eastern states until the following winter.
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Tamarack, California sits up in the Sierras of that state at an elevation of 6,913 feet. Located just south of Reno and Lake Tahoe it is home to one of the premiere ski venues in the United States and even the world for that matter, and for good reason. Snowfall averages an incredible 443” a year. Because of its location in the high Serra it is prone to getting hit by one strong pacific storm after another loaded with copious amounts of moisture that sometimes stream all the way from the central pacific. That moisture stream, often known as the Pineapple Express is a direct link all the way from the Hawaiian Islands and beyond. During the winter of 1911 the central part of California was impacted by one snowstorm after another. By March 11, 1911 snow on the ground measured an incredible 471” – the greatest snow depth ever measured in one place in the United States, a record that still holds today. Tamarack also holds the record for greatest seasonal snowfall in California: during the winter of 1906−1907, it received 883”. It’s no wonder so many skiers make the trip there every winter.
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Dust from the Sahara Desert in Africa is the main source of dust in the atmosphere on a yearly basis across the world. The dust has its origins principally in the remains of centuries old dry lake beds, mainly in the country of Chad. This dust is presentient and often times lifts into the low atmosphere creating a general haze across north central Africa. Because of its presence, storms and seasonal, or trade winds often pick up huge amounts of the dust and dirt and send it thousands of miles away from Africa – sometimes halfway around the world. The presence of the dust in Hurricane season can often act as a deterrent to the formation of tropical systems suppressing the formation of water droplets and clouds. Sometimes this dust makes it all the west into the Caribbean. It can cause travel disruptions diverting aircraft and interfering with radio waves. The most pronounced visible manifestation of the dust is in Europe. Often lifted high into the atmosphere from storms approaching the northwest coast of Africa or Portugal. The dust often settles into the lower atmosphere causing red sunrises and sunsets – but sometimes it’s washed out of the sky by rain and even more striking by snow. Such events, in the past, have resulted in superstitious approaches to the weather events. On March 10 1869 a reddish snow fell all day across central France. Some locals panicked because they thought it was colored in blood. Africans and scientists knew what the source of the red appearance was. The origin of the red color was the dust raised from the dry lake beds of Chad.
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The Battle of the Monitor and Merrimack occurred on March 9, 1862,. It was the first battle between ironclad warships. The Northern-built Merrimack, a conventional steam frigate, had been salvaged by the Confederates from the Norfolk navy yard. With her upper hull cut away and armored with iron, this 263-foot improvisation that resembled, according to one contemporary source, “a floating barn roof.” The ship had destroyed a fleet of wooden warships off Newport News, Virginia in the days leading up to the battle. The Union ironclad Monitor arrived the night of Marsh 8. This 172-foot “Yankee Cheese Box on a raft,” with its water-level decks and armored revolving gun turret, represented an entirely new concept of naval design. Thus the stage was set for the dramatic naval battle of March 9, with crowds of Union and Confederate supporters watching from the decks of nearby vessels and the shores on either side. They passed back and forth on opposite courses. Both crews lacked training; firing was ineffective. The Monitor could fire only once in seven or eight minutes but was faster and more maneuverable than her larger Confederate opponent. Both ships suffered some damage and retired. Because of the sheer weight of the ship and lack of maneuverability the previous days success of the Merrimac and the battle itself was only possible because of calm weather that allowed for smooth waters. In fact weather reports indicate the sky was clear and sunny with no wind. Even though the battle was inconclusive - it showed the superiority of the iron clad or metal covered ships and the engineering improved rapidly. Historians said that the battle made all navies that existed in the world at the time obsolete, and brought into existence modern naval warfare.
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