Eighteen Hundred and Froze to Death: The Eruption of Mt. Tambora

The year 1816 is known as the Year Without a Summer (also the Poverty Year, The Summer that Never Was, Year There Was No Summer, and Eighteen Hundred and Froze to Death), because of severe summer climate abnormalities that caused average global temperatures to decrease by 0.4–0.7 °C (0.7–1.3 °F). This resulted in major food shortages across the Northern Hemisphere. Evidence suggests that the anomaly was caused by a combination of a historic low in solar activity with a volcanic winter event, the latter caused by a succession of major volcanic eruptions capped by the 1815 eruption of Mount Tambora, in the Dutch East Indies (Indonesia), the largest known eruption in over 1,300 years. The Little Ice Age, then in its concluding decades, may also have been a factor. Caldera_Mt_Tambora_Sumbawa_Indonesia
The English governor of Indonesia, Sir Thomas Stamford Bingley Raffles, wrote of the erruption in his “History of Java” (1817). This was later incorporated in Lyell’s “Principles of Geology” (1850):

Island of Sumbawa, 1815. – In April, 1815, one of the most frightful eruptions recorded in history occurred in the province of Tomboro, in the island of Sumbawa, about 200 miles from the eastern extremity of Java. In the April of the year preceding the volcano had been observed in a state of considerable activity, ashes having fallen upon the decks of vessels which sailed past the coast. The eruption of 1815 began on the 5th of April, but was most violent on the 11th and 12th, and did not entirely cease till July.

The sound of the explosions was heard in Sumatra, at the distance of 970 geographical miles in a direct line; and at Ternate, in an opposite direction, at the distance of 720 miles. Out of a population of 12,000, in the province of Tomboro, only twenty-six individuals survived.

Violent whirlwinds carried up men, horses, cattle, and whatever else came within their influence, into the air; tore up the largest trees by the roots, and covered the whole sea with floating timber. Great tracts of land were covered by lava, several streams of which, issuing from the crater of the Tomboro mountain, reached the sea.

So heavy was the fall of ashes, that they broke into the Resident’s house at Bima, forty miles east of the volcano, and rendered it, as well as many other dwellings in the town, uninhabitable. On the side of Java the ashes were carried to the distance of 300 miles, and 217 towards Celebes, in sufficient quantity to darken the air. The floating cinders to the westward of Sumatra formed, on the 12th of April, a mass two feet thick, and several miles in extent, through which ships with difficulty forced their way.

The darkness occasioned in the daytime by the ashes in Java was so profound, that nothing equal to it was ever witnessed in the darkest night. Although this volcanic dust when it fell was an impalpable powder, it was of considerable weight when compressed, a pint of it weighing twelve ounces and three quarters.

“Some of the finest particles,” says Mr. Crawfurd, “were transported to the islands of Amboyna and Banda, which last is about 800 miles east from the site of the volcano, although the south-east monsoon was then at its height.” They must have been projected, therefore, into the upper regions of the atmosphere, where a counter current prevailed. Along the sea-coast of Sumbawa, and the adjacent isles, the sea rose suddenly to the height of from two to twelve feet, a great wave rushing up the estuaries, and then suddenly subsiding. Although the wind at Bima was still during the whole time, the sea rolled in upon the shore, and filled the lower parts of the houses with water a foot deep. Every prow and boat was forced from the anchorage, and driven on shore.

The town called Tomboro, on the west side of Sumbawa, was overflowed by the sea, which encroached upon the shore so that the water remained permanently eighteen feet deep in places where there was land before. Here we may observe, that the amount of subsidence of land was apparent, in spite of the ashes, which would naturally have caused the limits of the coast to be extended.

The area over which tremulous noises and other volcanic effects extended, was 1000 English miles in circumference, including the whole of the Molucca Islands, Java, a considerable portion of Celebes, Sumatra, and Borneo. In the island of Amboyna, in the same month and year, the ground opened, threw out water, and then closed again.

In conclusion, I may remind the reader, that but for the accidental presence of Sir Stamford Raffles, then governor of Java, we should scarcely have heard in Europe of this tremendous catastrophe. He required all the residents in the various districts under his authority to send in a statement of the circumstances which occurred within their own knowledge; but, valuable as were their communications, they are often calculated to excite rather than to satisfy the curiosity of the geologist. They mention, that similar effects, though in a less degree, had, about seven years before, accompanied an eruption of Carang Assam, a volcano in the island of Bali, west of Sumatra; but no particulars of that great catastrophe are recorded.

The Year Without a Summer was an agricultural disaster. Historian John D. Post has called this "the last great subsistence crisis in the Western world".The unusual climatic aberrations of 1816 had the greatest effect on most of New England, Atlantic Canada, and parts of western Europe. Typically, the late spring and summer of central and northern New England and southeastern Canada are relatively stable: temperatures (average of both day and night) average between about 68 and 77 °F (20 and 25 °C) and rarely fall below 41 °F (5 °C). Summer snow is an extreme rarity. 1816 summer temperature anomaly compared to average temperatures from 1971–2000. North America In the spring and summer of 1816, a persistent "dry fog" was observed in parts of the eastern U.S. The fog reddened and dimmed the sunlight, such that sunspots were visible to the naked eye. Neither wind nor rainfall dispersed the "fog". It has been characterized as a stratospheric sulfate aerosol veil. At higher elevations, where farming was problematic in good years, the cooler climate did not quite support agriculture. In May 1816, frost killed off most crops in the higher elevations of New England and New York. On June 4 frosts were reported as far south as northern Connecticut and the highlands of northwest New Jersey.  On June 6, snow fell in Albany, New York, and Dennysville, Maine. Many commented on the phenomenon. Sarah Snell Bryant, of Cummington, Massachusetts, wrote in her diary, "Weather backward." Thomas Dennis of Albany New York wrote to his son "We have had a cold wet season and every kind of fruits of the earth are backwards in Love". (Letter in collection of descendent Thomas Tailer.) At the Church Family of Shakers in upstate New York, near New Lebanon, Nicholas Bennet wrote in May 1816 that "all was froze" and the hills were "barren like winter." Temperatures went below freezing almost every day in May. The ground froze solid on June 9. On June 12, the Shakers had to replant crops destroyed by the cold. On July 7 it was so cold that everything had stopped growing. The Berkshire Hills had frost again on August 23, as did much of the upper northeast (MA, NH, VT, ME, upstate New York). A Massachusetts historian summed up the disaster:
"Severe frosts occurred every month; June 7th and 8th snow fell, and it was so cold that crops were cut down, even freezing the roots .... In the early Autumn when corn was in the milk it was so thoroughly frozen that it never ripened and was scarcely worth harvesting. Breadstuffs were scarce and prices high and the poorer class of people were often in straits for want of food. It must be remembered that the granaries of the great west had not then been opened to us by railroad communication, and people were obliged to rely upon their own resources or upon others in their immediate locality."
Farther north, nearly 12 inches (30 cm) of snow was observed in Quebec City in early June, with consequent additional loss of crops—most summer-growing plants have cell walls which rupture even in a mild frost. The result was regional malnutrition, starvation, epidemic, and increased mortality. In July and August, lake and river ice were observed as far south as Pennsylvania. Rapid, dramatic temperature swings were common, with temperatures sometimes reverting from normal or above-normal summer temperatures as high as 95 °F (35 °C) to near-freezing within hours. The weather was not in itself a hardship for those accustomed to long winters. The real problem lay in the weather's effect on crops and thus on the supply of food and firewood. Farmers south of New England did succeed in bringing some crops to maturity, but maize and other grain prices rose dramatically. The price of oats, for example, rose from 12¢ a bushel ($3.40/m³) in 1815, equal to $1.55 today, to 92¢ a bushel ($26/m³) in 1816 ($12.78 today). Crop failures were aggravated by an inadequate transportation network, with few roads or navigable inland waterways and no railroads; it was expensive to import food. Europe Cool temperatures and heavy rains resulted in failed harvests in Britain and Ireland. Families in Wales travelled long distances as refugees, begging for food. Famine was prevalent in north and southwest Ireland, following the failure of wheat, oats, and potato harvests. In Germany, the crisis was severe; food prices rose sharply. With the cause of the problems unknown, people demonstrated in front of grain markets and bakeries, and later riots, arson, and looting took place in many European cities. It was the worst famine of 19th-century Europe. Jane Austen even comments on the agricultural derth in a letter to her sister Cassandra,
We hear now that there is to be no honey this year. Bad news for us. We must husband our present stock of mead, and I am sorry to perceive that our twenty gallons is very nearly out. I cannot comprehend how the fourteen gallons could last so long... September 8, 1816
The effects were widespread and lasted beyond the winter. In eastern Switzerland, the summers of 1816 and 1817 were so cool that an ice dam formed below a tongue of the Giétro Glacier high in the Val de Bagnes. Despite engineer Ignaz Venetz's efforts to drain the growing lake, the ice dam collapsed catastrophically in June 1818, killing 44 people. Glacier_Giétro_-_Escher_von_der_Linth,_1818 Asia In China, the cold weather killed trees, rice crops, and even water buffalo, especially in the north. Floods destroyed many remaining crops. Mount Tambora's eruption disrupted China's monsoon season, resulting in overwhelming floods in the Yangtze Valley. In India the delayed summer monsoon caused late torrential rains that aggravated the spread of cholera from a region near the River Ganges in Bengal to as far as Moscow. Cause It is now generally thought that the aberrations occurred because of the April 5–15, 1815, volcanic Mount Tambora eruption on the island of Sumbawa, Indonesia (then part of the Dutch East Indies, but under French rule during Napoleon's occupation of the Netherlands), described by Thomas Stamford Raffles. The eruption had a Volcanic Explosivity Index ranking of 7, a super-colossal event that ejected immense amounts of volcanic ash into the upper atmosphere. It was the world's largest eruption since the Hatepe eruption in AD 180. That the 1815 eruption occurred during the middle of the Dalton Minimum (a period of unusually low solar activity) may also be significant.  Possible depiction of the eruption of the Tambora. Other large volcanic eruptions (with VEI at least 4) around this time were:
  • 1812, La Soufrière on Saint Vincent in the Caribbean
  • 1812, Awu in the Sangihe Islands, Indonesia
  • 1813, Suwanosejima in the Ryukyu Islands, Japan
  • 1814, Mayon in the Philippines
These eruptions had already built up a substantial amount of atmospheric dust. As is common after a massive volcanic eruption, temperatures fell worldwide because less sunlight passed through the stratosphere. According to a 2012 analysis by Berkeley Earth Surface Temperature, the 1815 Tambora eruption caused a temporary drop in the Earth's average land temperature of about 1 degree C. Smaller temperature drops were recorded from the 1812-1814 eruptions. Effects As a result of the series of volcanic eruptions, crops in the aforementioned areas had been poor for several years; the final blow came in 1815 with the eruption of Tambora. Europe, still recuperating from the Napoleonic Wars, suffered from food shortages. Food riots broke out in the United Kingdom and France, and grain warehouses were looted. The violence was worst in landlocked Switzerland, where famine caused the government to declare a national emergency. Huge storms and abnormal rainfall with flooding of Europe's major rivers (including the Rhine) are attributed to the event, as is the August frost. A major typhus epidemic occurred in Ireland between 1816 and 1819, precipitated by the famine the Year Without a Summer caused. It is estimated that 100,000 Irish perished during this period. A BBC documentary using figures compiled in Switzerland estimated that fatality rates in 1816 were twice that of average years, giving an approximate European fatality total of 200,000 deaths. New England also experienced major consequences from the eruption of Tambora. The corn crop was significantly advanced in New England and the eruption caused the crop to fail. It was reported that in the summer of 1816 corn ripened so badly that no more than a quarter of it was usable for food. The crop failures in New England, Canada and parts of Europe also caused the price of wheat, grains, meat, vegetables, butter, milk and flour to rise sharply. The eruption of Tambora also caused Hungary to experience brown snow. Italy's northern and northern-central region experienced something similar, with red snow falling throughout the year. The cause of this is believed to have been volcanic ash in the atmosphere. In China, unusually low temperatures in summer and fall devastated rice production in Yunnan, resulting in widespread famine. Fort Shuangcheng, now in Heilongjiang, reported fields disrupted by frost and conscripts deserting as a result. Summer snowfall or otherwise mixed precipitation was reported in various locations in Jiangxi and Anhui, located at around 30 degrees latitude. In Taiwan, which has a tropical climate, snow was reported in Hsinchu and Miaoli, and frost was reported in Changhua. Cultural effects High levels of tephra in the atmosphere led to unusually spectacular sunsets during this period, a feature celebrated in the paintings of J. M. W. Turner (baptised 14 May 1775 – 19 December 1851). It has been theorised that it was this that gave rise to the yellow tinge that is predominant in his paintings such as Chichester Canal circa 1828. Similar phenomena were observed after the 1883 eruption of Krakatoa and on the West Coast of the United States following the 1991 eruption of Mount Pinatubo in the Philippines. Hong Kong sunset c. 1992 after the eruption of Mount Pinatubo. The lack of oats to feed horses may have inspired the German inventor Karl Drais to research new ways of horseless transportation, which led to the invention of the draisine or velocipede. This was the ancestor of the modern bicycle and a step toward mechanized personal transport. Drais' Laufmaschine 1817.   The crop failures of the "Year without a Summer" may have helped shape the settling of the "American Heartland", as many thousands of people (particularly farm families who were wiped out by the event) left New England for what is now western and central New York and the Midwest (then the Northwest Territory) in search of a more hospitable climate, richer soil, and better growing conditions. According to historian L.D. Stillwell, Vermont alone experienced a drop of between 10,000 and 15,000 people, erasing seven previous years of population growth.Among those who left Vermont were the family of Joseph Smith, who moved from Sharon, Vermont, to Palmyra, New York. This move precipitated the series of events that culminated in the publication of the Book of Mormon and the founding of the Church of Jesus Christ of Latter-day Saints. In June 1816 "incessant rainfall" during that "wet, ungenial summer" forced Mary Shelley, John William Polidori, and their friends to stay indoors for much of their Swiss holiday. They decided to have a contest to see who could write the scariest story, leading Shelley to write Frankenstein, or The Modern Prometheus and Lord Byron to write "A Fragment", which Polidori later used as inspiration for The Vampyre — a precursor to Dracula. In addition, Lord Byron was inspired to write a poem, Darkness, at the same time.
I had a dream, which was not all a dream. The bright sun was extinguish’d, and the stars Did wander darkling in the eternal space, Rayless, and pathless, and the icy earth Swung blind and blackening in the moonless air; Morn came and went – and came, and brought no day” “Darkness” (1816) by Lord Bryon (1788-1824)  
Text and images from Wikipedia.com

3 comments

There are different kind of trees in the world trees like deciduous trees, coniferous trees, arborvitae, banyan trees, black Ash, white Ash, and many others. I thing the tallest tree in the world is Hyperion which is over 300 feet tall (91 meters) . The tallest tree in the world is located in California it has been standing over 700/800 years old. Hyperion is also known as coast redwood. while the smallest tree in the world is dwarf willow it dose not grow more then 1-6 cm it is mainly located in North Atlantic Ocean it is one of the smallest of woody plants. I really love trees and plant thanks for this article.

precious August 17, 2020

There are different kind of trees in the world trees like deciduous trees, coniferous trees, arborvitae, banyan trees, black Ash, white Ash, and many others. I thing the tallest tree in the world is Hyperion which is over 300 feet tall (91 meters) . The tallest tree in the world is located in California it has been standing over 700/800 years old. Hyperion is also known as coast redwood. while the smallest tree in the world is dwarf willow it dose not grow more then 1-6 cm it is mainly located in North Atlantic Ocean it is one of the smallest of woody plants. I really love trees and plant thanks for this article.

precious August 17, 2020

There are different kind of trees in the world trees like deciduous trees, coniferous trees, arborvitae, banyan trees, black Ash, white Ash, and many others. I thing the tallest tree in the world is Hyperion which is over 300 feet tall (91 meters) . The tallest tree in the world is located in California it has been standing over 700/800 years old. Hyperion is also known as coast redwood. while the smallest tree in the world is dwarf willow it dose not grow more then 1-6 cm it is mainly located in North Atlantic Ocean it is one of the smallest of woody plants. I really love trees and plant thanks for this article.

precious August 17, 2020

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