and probably saved
a substantial number of lives on the more distant islands as the rain washed the ash
off crops and provided fresh drinking water to help stem an incipient epidemic of
fever. But nothing could save those closer to Tambora. Over the following month, thousands
more perished—some from severe respiratory infections from the ash that remained in
the atmosphere in the aftermath of the eruption, others from violent diarrhoeal disease,
the result of drinking water contaminated with acidic ash. The same deadly ash poisoned
crops, especially the vital rice fields, raising the death toll higher. Horses and
cattle perished by the hundreds, mainly from a lack of forage. Lieutenant Owen Phillips,
dispatched by Raffles to investigate conditions and provide an emergency supply of
rice to the inhabitants, arrived in Bima several weeks after the eruption and reported
that “the extreme misery to which the inhabitants have been reduced is shocking to
behold. There were still on the road side the remains of several corpses, and the
marks of where many others had been interred: the villages almost entirely deserted
and the houses fallen down, the surviving inhabitants having dispersed in search of
food.” In the nearby village of Dompo, residents were reduced to eating stalks of
papaya and plantain, and the heads of palm. Even the Raja of Sanggar lost a daughter
to hunger.
In the end, perhaps another seventy to eighty thousand people died from starvation
or disease caused by the eruption, bringing the death toll to nearly ninety thousand
in Indonesia alone. No other volcanic explosion in history has come close to wreaking
disaster of that magnitude.
And yet there would be more casualties from Tambora. In addition to millions of tons
of ash, the force of the eruption threw 55 million tons of sulfur-dioxide gas more
than twenty miles into the air, into the stratosphere. There, the sulfur dioxide rapidly
combined with readily available hydroxide gas—which, in liquid form, is commonly known
as hydrogen peroxide—to form more than 100 million tons of sulfuric acid. The sulfuric
acid condensed into minute droplets—each two hundred times finer than the width of
a human hair—that could easily remain suspended in the air as an aerosol cloud. The
strong stratospheric jet streams quickly accelerated the particles to a velocity of
about sixty miles per hour, blowing primarily in an east-to-west direction. The sheer
power of the jet stream allowed the aerosol cloud to circumnavigate Earth in two weeks;
but the cloud did not remain coherent.
Variations in the wind speed and the weight of the particles caused some parts of
the cloud to travel faster or slower than others, and so the cloud spread as it moved
around Earth, until it covered the equator with an almost imperceptible veil of dust
and sulfurous particles. It also began to spread north and south, albeit far more
slowly. While it took only two weeks for the aerosol cloud to cover the globe at the
equator, it was likely more than two months before it reached the North and South
Poles.
Rather than a slow, steady broadening of the equatorial cloud into the Northern and
Southern Hemispheres, the cloud expanded in fits and starts. As some pieces of the
cloud were blown away from the equator, they were quickly caught up in the dominant
stratospheric jet streams—which in May blow east to west in the Northern Hemisphere,
and west to east in the Southern Hemisphere. The cloud soon began to resemble streamers
or filaments, with small portions regularly pushed off the equator and into the middle
latitudes in each hemisphere. Eventually, these filaments coalesced into a single,
coherent cloud that covered Earth.
And there they remained. Had the aerosol cloud ascended only into the lowest part
of the atmosphere, the troposphere, where clouds form, rain would soon have cleansed
the ash from the