How Volcanoes Affect Our Climate

Big, explosive eruptions can send huge quantitiesbe seen was a blanket of ash. A
of gas and fine debris into the atmosphere. Thehorseshoe-shaped crater 1.2 miles across and
bigger ones have sent debris high into theroughly 2460 feet deep replaced the peak. But
stratosphere where it spreads around the globethe most impressive thing was the blowdown
and might remain for months or even years. Thezone where huge virgin Douglas firs were snapped
debris has the ability to filter out a portion of thelike matchsticks and lay on their sides, covered
sun's energy and to lower the earth'swith ash. The U.S. Forest Service estimated that
temperature.The most notable cold spell linked to10 million trees were felled by the blast.When
a volcano was the one that followed the eruptionMount St. Helens Erupted, there was instant
of Mount Tambora in Indonesia in 1815. Manyspeculation that it could have major effects on
scientists attribute the abnormally cold spring andclimate. For a time the large volume of volcanic
summer of 1816 to the clouds of volcanic debrisash that it emitted had significant effects both
put into the atmosphere by Mount Tambora.locally and regionally. But worldwide cooling was
There were other less dramatic effects fromless than 0.2 degrees Fahrenheit.However, studies
Kakatoa in 1883 and Mount Agung in 1963.following the eruption of El Chichon showed a
However, it wasn't until the eruptions of Mount St.worldwide cooling effect on the order of .5 to .9
Helens in the state of Washington in 1980 and Eldegrees Fahrenheit. Why, if it was less explosive
Chichon in Mexico in 1982 that scientists really gotthan Mount St. Helens, did it have a greater
to study the volcanic blasts with the use ofimpact on global temperatures? The reason is
sophisticated satellites and remote sensingthat the material emitted by Mount St. Helens
instruments.Prior to 1980, Mount St. Helens,was fine ash that settled out relatively quickly. El
Washington was a steep conical volcanic peakChichon, on the other hand, spewed an estimated
that rose 9,680 feet, had a snow-capped summit40 times more sulfur-rich gases than Mount St.
and even a few small glaciers. But on the morningHelens. These clouds combined with moisture in
of May 18th, 1980, the entire north side of thethe stratosphere to produce dense clouds of
summit came down - about half a cubic mile ofsulfur acid droplets, which both absorbed and
rock and ice. An instant later and enormousreflected solar radiation. Explosiveness alone is a
explosion of expanding steam and volcanic gaspoor instigator of climatic change. For volcanism to
rocked the countryside. The gases formed aimpact the climate, you would have to have a
ground-hugging black cloud filled with hot, densewhole bunch of volcanoes going off over a
debris that raced over four major ridges andrelatively short period of time. Such an idea was
valleys up to 17 miles from the volcaniconce floated as the reason for the ice ages, but
summit.For the first couple of miles from thescientists have other ideas today.
summit, everything was obliterated. All that could