The Unlikely Record · Episode 15 · Twelve stories
Twelve interruptions recorded in clouds, ice, instruments and altered plans
Weather can suspend an ordinary errand or alter a decision involving thousands of people. These twelve records follow the interruption beyond its first dramatic moment: a writing challenge, a failed warning light, a press on a frozen river, and investigators separating observation from explanation. Some events were forecasts; others only became understandable when later evidence could be compared.
Story 01
Rain at the Writing Table
A Swiss holiday produced an unusually durable souvenir. In the summer of 1816, eighteen-year-old Mary Godwin, later Mary Shelley, stayed near Lake Geneva in a circle that included Percy Shelley, Lord Byron and John Polidori. Rain repeatedly confined them indoors. The weather interrupted excursions, leaving time for conversation and the reading of ghost stories.
In the introduction she wrote for Frankenstein in 1831, Mary recalled Byron proposing that each of them write a frightening tale. Her contribution did not arrive instantly. She remembered successive mornings when she still had nothing to report, followed by discussions about life, manufactured bodies and the possibility of reanimation. An unsettling waking vision supplied the central image she wanted.
That wet summer belonged to a larger climatic disturbance following the enormous 1815 eruption of Tambora, in what is now Indonesia. The Science Museum places the Geneva gathering within this cooling episode. The connection joins a distant eruption to the conditions of a European visit; it cannot account for the particular story Mary made from her reading and thought.
Her later introduction also resists the impression of a finished novel arriving in one night. She described beginning with a short tale and developing it further. The rain helped rearrange a holiday. The sustained work of an author turned that altered schedule into Frankenstein.
Evidence and sources
The visit and novel’s origin are documented. The author’s detailed account is retrospective, and weather supplies context rather than a complete explanation of creativity.
- Frankenstein, 1831 author’s introduction — Mary Shelley; Project Gutenberg transcription
Introduction, account of Switzerland in 1816 - The Creation of Frankenstein — Science Museum
Story 02
A Fog That Would Not Burn Away
The unusual European haze of 1783 bothered Benjamin Franklin because it behaved differently from ordinary fog. Sunshine did not readily clear it. In a paper dated May 1784, he described rays so weakened that a burning glass struggled to ignite brown paper. The puzzle was practical as well as philosophical: could such a summer warn people of a damaging winter?
Franklin proposed that reduced summer heating had allowed the ground to freeze sooner, leaving snow in place and intensifying the cold. For the haze itself, he offered alternatives. One involved material from burning celestial bodies. Another involved prolonged volcanic activity around Iceland. He explicitly acknowledged that the cause had not yet been established.
Later research connected the dry haze with the Laki fissure eruption in southern Iceland and its sulfurous aerosols. That association does not settle every consequence. A 2011 study tested atmospheric circulation as an alternative explanation for the severe winter, arguing that natural variability was its dominant cause. Historical sequences can be clear even when the balance of causes remains difficult to reconstruct.
Franklin ended with a proposal for comparison: investigate whether other severe winters had followed widespread summer haze. His paper preserves the moment observation became a question for further records. A frightening sky prompted a useful investigation without supplying an instantly complete answer.
Evidence and sources
The haze is documented and linked to Laki. Franklin’s explanation of the next winter was a contemporary hypothesis; its climatic attribution remains debated.
- Meteorological Imaginations and Conjectures, May 1784 — Benjamin Franklin; National Archives / Franklin Papers
Final paragraphs on the dry fog and the following winter - The Great Dry Fog of 1783 — NASA Goddard Institute for Space Studies / R. B. Stothers
Complete abstract of the 1996 paper - The anomalous winter of 1783–4: Was the Laki eruption or an analog of the 2009–10 winter to blame? — NASA GISS / D’Arrigo and colleagues
Complete abstract of the 2011 paper
Story 03
The Light Disappeared
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A lighthouse is built to remain visible when everything around it becomes difficult to read. Henry Winstanley’s tower on the Eddystone Rocks made an especially ambitious promise. Completed in 1698, it marked a dangerous reef in the open sea off Plymouth. Its builder had earned money from elaborate mechanical entertainments, then invested in a structure meant to protect passing ships.
The first winter exposed the tower’s vulnerability. Keepers reported breakers overtopping it, and Winstanley enlarged and strengthened his design. A painting held at Mount Edgcumbe records the revised structure: an intricate, conspicuous building rising from a very small foundation in the sea. Its painter is unidentified, despite suggestions that Winstanley might have made it himself.
In November 1703, Winstanley was on the rock supervising repairs when the great storm arrived. When vessels could approach afterward, the lighthouse had vanished. Winstanley had died with it. The very place intended to give mariners warning had become a place from which its occupants could not escape.
The loss did not end the attempt to mark Eddystone. A new tower was lit in 1709, followed by further replacements. Those successive structures make the disaster part of an engineering history as well as a storm story: early confidence encountered conditions that forced later builders to rethink how a light could hold its ground.
Evidence and sources
The tower’s loss with Winstanley is documented. Popular heroic quotations and supposed supernatural omens are omitted.
- Eddystone Lighthouse — Trinity House
Tower chronology - Winstanley’s Light, painting 1699–1703 — Mount Edgcumbe
Anonymous painting and tower alterations
Story 04
Printed on a River
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For a brief interval in 1814, a London customer could buy a printed souvenir whose selling point was its unlikely place of manufacture. The press stood on the Thames. Severe cold had turned part of the working river into the site of a frost fair, with temporary booths and entertainments occupying space normally used by boats.
The Bodleian’s John Johnson Collection preserves the paper trail. Its catalogue lists a handbill printed near Thames Street Stairs at Bankside on 4 February, keepsakes carrying customers’ names, and small papers intended for watches. One surviving sheet bears a handwritten note explaining that its owner’s father had watched it being printed on the river. The object records both the spectacle and a family’s effort to remember it.
A contemporary view in Royal Museums Greenwich shows musicians, refreshment tents and children at play. Published in May, it depicts the fair of early February. That difference between the event and the print’s production matters: a picture could continue selling the experience after the ice had gone.
The museum also points out who lost from this temporary transformation. A frozen Thames disrupted the port. The same surface that gave stallholders new premises interrupted other people’s work. Surviving keepsakes capture an ingenious business opportunity created by weather, while leaving much of the wider economic inconvenience outside their cheerful borders.
Evidence and sources
Contemporary prints and surviving souvenirs document commerce and printing on the frozen river; celebratory images give a partial view of the disruption.
- John Johnson Collection: Printed on the Ice — Bodleian Libraries
Page 2, 1814 frost fair souvenirs - The Fair on the Thames, Feby. 4. 1814, PAH9908 — Royal Museums Greenwich
Print description and creation date, 1 May 1814
Story 05
When the Air Stopped Moving
Londoners were accustomed to fog, but the air that settled over the city in December 1952 made familiar journeys impossible. Visibility fell to a few metres. In the Isle of Dogs, the Met Office records conditions so dense that pedestrians could not see their own feet. Buses and ambulances were taken off the roads while people struggled to reach help.
Cold weather had increased the need for heating in a city heavily dependent on coal. Smoke from homes, factories and power generation accumulated beneath an atmospheric inversion. Warmer air above held cooler air near the ground, and weak winds failed to disperse the pollution. Ordinary efforts to keep warm fed a dangerous concentration of contaminants in the air people had to breathe.
The fog cleared on 9 December, but the deaths could not be counted simply by looking at the streets afterward. Thousands died; later estimates extend beyond the early count to include further premature deaths. The difficulty of defining a total does not make the public-health catastrophe uncertain.
The Clean Air Act of 1956 became part of the response, with restrictions on smoke and changes to fuels. Improvement took time, and another deadly fog occurred in 1962. London’s interruption exposed a dependency that legislation and infrastructure had to change long after the weather itself moved on.
Evidence and sources
The event, pollution mechanism and legislative response are documented. Death estimates depend on the period and method counted.
- The Great Smog of 1952 — Met Office
5–9 December conditions, inversion and response - Power up: energy use — UK Parliament / Olympic Britain
London coal use and the 1952 smog
Story 06
The Winter Beyond the Holiday
A white Christmas could be treated as a seasonal novelty. The winter that began around Christmas 1962 refused to end with the holiday. Cold easterly air arrived before the festivities, followed by snow reaching southern England on Boxing Day. Blizzards on 29 and 30 December built deep drifts across Wales and the southwest.
Roads and railway lines became obstructed, telephone connections failed, and some villages were isolated for days. Farmers struggled to reach animals. In much of England, the snow already on the ground remained through the following two months. Bright sunshine could make the landscape look inviting while weak winter heating and clear nights helped preserve the cold.
The transport effort also entered the film record. Geoffrey Jones directed Snow, an eight-minute film produced by Edgar Anstey in 1963. British Transport Films existed partly to explain the network’s work to its employees and passengers. A weather emergency therefore became material for an institution whose public promise depended on movement.
A milder southwesterly flow finally arrived in early March. The episode shows how a short weather forecast and a long disruption can belong to different timescales. Once deep snow had accumulated, daily life depended on the continued effort to clear routes and maintain supplies. A change in the wind was only the beginning of getting the timetable back.
Evidence and sources
Meteorological records establish the long freeze; film catalogue records document a contemporary transport response without making the film a complete national survey.
- Severe Winters — Met Office
The winter of 1963; not the separate 1947 section - Snow (1963) — British Film Institute
Director, producer, year and eight-minute duration - Where to begin with British Transport Films — British Film Institute
British Transport Films purpose and Geoffrey Jones films
Story 07
A Forecast for One More Day
An invasion assembled on an enormous scale still depended on a small opening in the weather. Allied planners intended to land in Normandy on 5 June 1944. Forecasts discussed during the night of 3–4 June made conditions look too dangerous, and Dwight Eisenhower postponed the operation. Waiting solved the immediate problem while creating another: the force needed a usable date soon.
James Stagg coordinated advice from three forecasting teams representing the Met Office, Admiralty and United States Army Air Forces. They did not begin with complete agreement. Charts were drawn by hand from observations gathered across a wartime network. Wind, visibility, cloud and sea conditions mattered differently to ships, aircraft and troops, making a simple declaration of good weather inadequate.
The next forecast discussions identified a limited improvement for 6 June. Conditions would still fall short of the ideal, but they offered an opportunity the commanders accepted. The landings went ahead. The useful forecast promised a workable interval rather than a calm, uncomplicated day.
Modern researchers have reconstructed the weather using surviving observations and newer models. Those reconstructions help examine the decision without placing modern tools in Stagg’s hands. His team worked with incomplete information and a moving deadline. Their contribution lay in making uncertainty usable for a commander who could delay the timetable, but could not control the Channel.
Evidence and sources
Forecast records and institutional research establish the decision sequence. Later computer reanalyses reconstruct the weather using information and methods that were unavailable to the forecasters in 1944.
- D-Day: the most important weather forecast in history — Met Office
Historical charts and James Stagg’s team - D-Day Analyses — European Centre for Medium-Range Weather Forecasts
Introduction and contemporary forecast decisions
Story 08
Keeping Station in a Typhoon
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Fuel had become an urgent problem for ships of Admiral William Halsey’s Third Fleet in December 1944. Sustained operations off the Philippines had depleted supplies, but worsening seas made refuelling dangerous. Hoses parted and vessels risked colliding. Manoeuvres intended to find better conditions brought elements of the fleet into the path of a powerful typhoon.
On 18 December, the destroyers Hull, Monaghan and Spence sank. Low fuel could leave ships less stable unless ballast replaced the missing weight; efforts to remain in formation could also put a vessel at a dangerous angle to the sea. The disaster joined limited warning, difficult decisions and ships’ physical vulnerabilities. Roughly 790 sailors died across the force.
The destroyer escort Tabberer had lost its foremast and radio antennas but encountered a survivor that evening. Lieutenant Commander Henry L. Plage began a search despite his own ship’s damage. Over the following 51 hours, Tabberer rescued 55 men. The search turned a crippled escort into a means of survival for others.
A Court of Inquiry convened at Ulithi on 26 December. It assigned responsibility for the losses to Halsey while describing his decisions as errors of judgment rather than negligence. It also examined the delay in abandoning formation. Keeping a fleet together had been a military discipline; in this storm, individual ships needed room to survive.
Evidence and sources
Naval histories document the losses, rescue and inquiry. Uncertain claims about deliberate disobedience and inconsistent survivor totals are omitted.
- H-039-2: Typhoon Cobra Overview — Naval History and Heritage Command / Samuel J. Cox
Storm, low fuel, Tabberer and Court of Inquiry - Haggard (DD-555) — Naval History and Heritage Command
December 1944 war-diary extracts
Story 09
The Coal Could Not Arrive
By the time the snow stopped in Albany in March 1888, the official storm total had reached 46.7 inches. The depth was impressive, but the consequences were measured in more ordinary things: coal that could not be delivered, doctors unable to make house calls, and roads requiring days of work before people could pass.
The National Weather Service’s reconstruction follows a storm that developed over northern Georgia on 11 March, moved offshore, and then stalled near southern New England. Snow began in Albany on Sunday and intensified overnight. By Monday morning, approximately eighteen inches lay on the ground. Further snowfall and drifting made an already difficult journey worse.
Across the northeast, contemporary newspapers described damaged communications and stranded transport. The Sun’s front page on 13 March treated the metropolis as helpless under snow. A network designed to link distant places now depended on clearing small, obstructed stretches of track and street. The storm exposed how fuel, food, information and medical care all relied on movement.
Albany’s total belongs to Albany; other places experienced different accumulations and hazards. That local measurement is more revealing than a single exaggerated number for the whole region. The city had not lost the existence of coal or medical knowledge. It had temporarily lost reliable ways of bringing essential supplies and people to the doors where they were needed.
Evidence and sources
This is the March coastal blizzard, a distinct event from the previously covered January 1888 Children’s Blizzard. Snow totals are attached to their recorded location.
- Past Weather Events: The Blizzard of 1888 — National Weather Service, Albany
The Blizzard of 1888 (March 11–14), Albany observations - Great Blizzard of 1888: Topics in Chronicling America — Library of Congress
Introduction and contemporary newspaper link
Story 10
The Explosion Arrived on Paper
A volcano in the Sunda Strait left traces on instruments far beyond the places that heard its explosions. Krakatau’s eruption reached its catastrophic peak on 27 August 1883. Along with the devastating local effects, an atmospheric pressure disturbance travelled outward. Recording barometers turned its passage into marks that could later be compared across great distances.
The Royal Society established a committee to collect authenticated observations. Its request was unusually wide-ranging: dust and pumice, sea levels, pressure changes, sounds, and strange atmospheric colours. Ship captains and observers on land supplied letters, records and specimens. Material gathered for one purpose became evidence for a connected event that no single witness could see in full.
The committee’s 1888 report mapped the pressure wave using observations from approximately fifty stations worldwide. Its movement could be followed across the globe and toward the opposite side of the Earth. Meanwhile, William Ascroft recorded vivid sunset effects from Chelsea in November 1883. The instrument trace and the painted sky preserved different aspects of the same far-reaching disturbance.
Collecting these observations did not erase the destruction near Krakatau. It changed the scale at which investigators could understand it. A local catastrophe had produced a distributed archive: lines on paper, coloured studies, ships’ logs and pieces of floating pumice. The atmosphere had carried the disturbance; people then had to assemble the record.
Evidence and sources
The eruption and distant atmospheric observations are documented. Individual visual and sound reports require their own dates and attribution.
- Crowdsourcing Krakatoa — Royal Society
Committee call, letters, Ascroft observations and 1888 report - Krakatau pressure-wave maps and the 1888 report — Kevin Hamilton, University of Hawaiʻi at Mānoa
Krakatau passage and description of approximately 50 barometric stations
Story 11
Candles Before Lunch
Cotton Tufts could no longer read or write without a candle by late morning on 19 May 1780. In the account he sent to John Adams, he described darkness deepening over New England, oddly coloured clouds and a smell that reminded people of burning chimneys or swamps. The practical interruption arrived before any agreed explanation.
His document preserves different responses. Some people looked to comets, planets or catastrophe. Tufts proposed smoke carried by winds and concentrated by the morning’s weather. He also included observations made elsewhere, including an Ipswich meal taken with candles burning. These were comparisons assembled by a contemporary investigator, rather than one observer miraculously describing an entire region.
More than two centuries later, researchers added another kind of record. Fire scars in trees from Ontario’s Algonquin Highlands could be dated to 1780. In some samples, the position of the injury within the annual growth indicated an early-season fire, consistent with May. Written weather accounts and the physical evidence made distant wildfire smoke a strong explanation for the darkness.
The study allowed that fires in other areas might also have contributed. It did not identify a single proven ignition or remove every uncertainty about the smoke’s route. The unusual day survives through two archives that were never designed to work together: people’s descriptions of a dimmed sky and injuries retained in growing wood.
Evidence and sources
Eyewitness darkness is documented. Tree-ring research supports distant fires as the likely cause without proving one exact source or ignition.
- Account of the Dark Day in May 1780 — Cotton Tufts; National Archives / Adams Papers
Complete enclosure addressed to John Adams - Fire scars reveal source of New England’s 1780 Dark Day — McMurry, Stambaugh, Guyette and Dey; US Forest Service repository
Pages 266–269, dating, likely source and other possible contributing fires
Story 12
The Cold After the Wave
An unusually mild January day ended in disaster on Boston’s waterfront. On 15 January 1919, a large storage tank released roughly 2.3 million gallons of industrial molasses into the North End. Buildings and railway structures were damaged, and people were caught in a substance whose familiar use in food gave little warning of its force at that scale.
Twenty-one people died. Police, Red Cross workers and cadets from the nearby Nantucket joined the rescue. The tank had leaked before the collapse, and the legal investigation turned toward its construction and ownership. In 1925, a court-appointed auditor attributed the disaster to the owners’ negligence. A pleasant change in weather did not remove responsibility for a dangerous structure.
Researchers later examined what happened to the molasses after release. In work presented in 2016, Nicole Sharp, Jordan Kennedy and Shmuel Rubinstein combined historical records with experiments on flow. Cooling made the substance much more viscous. Molasses recently delivered from the Caribbean was probably warmer than the outside air, so spreading it through cold streets could greatly change its behaviour.
That analysis helps explain why a fast-moving disaster could leave such difficult rescue conditions. As temperatures dropped, the material could become harder to move through and clear away. The weather belongs in the account as part of the aftermath and physical setting, alongside the documented failure of the tank.
Evidence and sources
The tank failure and deaths are documented. Later viscosity research helps explain spreading and rescue conditions; it does not establish weather as the sole cause of collapse.
- Molasses crashes through Boston’s North End — Boston City Archives / City of Boston
Tank, casualties, rescue and 1925 ruling - Molasses Creates a Stick Situation: Physics Meets History — American Physical Society / American Institute of Physics
21 November 2016, pages 1–2
An altered sky rarely acts alone. It meets buildings, fuel supplies, institutions and people making decisions with the information they have. The surviving records show both the force of those encounters and the care needed to explain them.
About the evidence labels
Documented identifies a supported historical event. Disputed marks an account whose explanation or details remain contested. Folklore identifies a recorded tradition; its inclusion does not establish that a supernatural event occurred.
