Description: Mount Tambora, a stratovolcano in Sumbawa, Indonesia became highly active in 1812 and erupted again on April 5th and April 10th, 1815. The major blast on the 10th was heard from 1,600 miles away and was thought to be the sound of firing cannonade. The eruption was four times larger than Krakatoa's in 1883. Pyroclastic flows spread at least 12 miles from the summit and killed an estimated 10,000 people. The eruption column reached the stratosphere - at an altitude of more than 140,000 feet. The coarser ash particles fell one to two weeks after the eruptions, but the finer ash particles stayed in the upper atmosphere from a few months up to a few years. Longitudinal winds spread these fine particles around the globe, creating optical phenomena that bore prolonged and brilliantly colored sunsets. The unusual climatic aberrations of 1816 had the greatest effect on the Northeastern United States, New England, the Canadian Maritimes, Newfoundland and Northern Europe.
But there were two other factors, that factored with the Tambora eruption, caused sensational unseasonable temperature drops around the world. Sustained periods of weak magnetic activity make the Sun slightly dimmer, so Earth receives less solar light energy. The years 1812-15 were nearly ‘spotless’. The year 1816 had a rash of sunspots in the Spring with two major periods of solar activity - from May 3rd through May 10th, 1816 and again on June 11th, 1816. These could easily be seen with the naked eye at sunset. Many attributed the dank weather to the sunspots due to “lessening the amount of sunlight that was reaching the earth” – which was, of course, the opposite result. Solar irradiance actually increases with sunspot activity.
A third factor was 'inertial solar motion' - which is the shifting of the sun's position within our solar system in relation to the earth's revolution around the sun.
The temperature shifts were dramatic. In May 1816, frost killed off most of the crops that had been planted in New England. In June, two large snowstorms in eastern Canada and New England resulted in many human deaths. Nearly a foot of snow was observed in Quebec City in early June, with the consequential loss of crops. The result was regional malnutrition, starvation, epidemic, and increased mortality — in short, famine.
In July and August, lake and river ice was 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) to near-freezing within hours.
Even though farmers south of New England did succeed in bringing some crops to maturity, maize and other grain prices rose dramatically. Those areas suffering local crop failures had to deal with the lack of roads in the early 19th century, which prevented easy importation of bulky food stuffs. Many New England farmers were wiped out and tens of thousands struck out for the richer soil and better growing conditions of the Upper midwest (then the Northwest Territory). The winter of 1816-17 was brutal. There were luminous (electrical) snowstorms (‘thundersnow’) in Vermont in January and February of 1817 where ball lighting shocked many people.
Join historical astronomer and weather historian John Horrigan as he takes you through the "Year Without a Summer" and parallels it with the current aberrational weather conditions and dormant sunspot period.