Pinatubo91_lateral_blast_plume_pinatubo_06-15-91.jpg
View to west from Clark Air Base of Pinatubo's lateral blast cloud of eruption of 5:55 am.
U.S. Geological Survey Photograph taken on June 15, 1991, by Rick Hoblitt.
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From:
Richard S. Williams, Jr.,
Glaciers: Clues to Future Climate:
USGS General Interest Publication, 1999 Online version
Among the more prominent theories of events that have triggered
global climatic changes and lead to repeated glaciation are: (1) known
astronomical variations in the orbital elements of the Earth (the so-called
Milankovitch theory); (2) changes in energy output from the Sun; and (3)
increases in volcanism that could have thrown more airborne volcanic
material into the stratosphere, thereby creating a dust veil and lowered
temperatures.
The years 1980, 1981, and 1982, for example, saw several major volcanic
eruptions adding large quantities of particulate volcanic material
and volatiles to the stratosphere, including the catastrophic eruption of
Mount St. Helens, Washington, on May 18, 1980,
and a large eruption of
Mount Hekla, Iceland, on August 17, 1980.
The 1982 series of eruptions from
El Chichón volcano, Mexico,
caused death and destruction in the
populated area around the volcano, but a further reaching impact may
result from the effect on Earth's climate because of the enormous ejection
of volcanic material into the stratosphere.
The potential climatic effect of the
Laki volcanic eruption in Iceland in 1783,
the largest effusive (lava) volcanic eruption in historic time, was
noted by the diplomat-scientist Benjamin Franklin in 1784, during one of
his many sojourns in Paris. Franklin concluded that the introduction of
large quantities of volcanic particles into the Earth's upper atmosphere
could cause a reduction in surface temperature, because the particles
would lessen the amount of solar energy reaching the Earth's surface. The
catastrophic eruption of the
Tambora volcano, Indonesia, in 1815
was followed
by a so-called "year-without-a-summer." In New England, for
example, frost occurred during each of the summer months in 1816.
From:
Kious and Tilling, 1996,
This Dynamic Earth: The Story of Plate Tectonics:
USGS General Interest Publication
The
June 1991 eruption of Mount Pinatubo
was global.
Slightly cooler than usual temperatures recorded worldwide
and the brilliant sunsets and sunrises have been attributed to this eruption
that sent fine ash and gases high into the stratosphere, forming a large
volcanic cloud that drifted around the world. The sulfur dioxide (SO2)
in this cloud -- about 22 million tons -- combined
with water to form droplets of sulfuric acid, blocking some of the
sunlight from reaching the Earth and thereby cooling
temperatures in some regions by as much as 0.5 degrees C. An eruption the
size of Mount Pinatubo could affect the weather for a few years.
A similar phenomenon occurred in April of 1815 with the
cataclysmic eruption of Tambora Volcano in Indonesia,
the most powerful eruption in recorded history.
Tambora's volcanic cloud lowered global temperatures by as
much as 3 degrees C.
Even a year after the eruption, most of the
northern hemisphere experienced sharply cooler temperatures
during the summer months. In parts of Europe and in North America,
1816 was known as "the year without a summer."
From:
NASA's Earth Observing Project Science Webpage:
Volcanoes and Global Climate Change, May 2000
Volcanic eruptions are thought to be responsible for the global cooling that has been observed for a few years
after a major eruption. The amount and global extent of the cooling depend on the force of the eruption and,
possibly, its latitude. When large masses of gases from the eruption reach the stratosphere, they can produce a
large, widespread cooling effect. As a prime example, the effects of
Mount Pinatubo,
which erupted in June 1991, may have lasted a few years, serving to offset temporarily the predicted greenhouse
effect.
Global cooling often has been linked with major volcanic eruptions. The year 1816 often has been
referred to as "the year without a summer". It was a time of significant weather-related disruptions in New
England and in Western Europe with killing summer frosts in the United States and Canada. These strange
phenomena were attributed to a major eruption of the
Tambora volcano in 1815 in Indonesia.
The volcano threw sulfur dioxide gas into the stratosphere, and the
aerosol layer that formed led to brilliant sunsets seen around the world for several years.
However, there is some confusion about the historical evidence that global cooling may be caused by
volcanic emissions. Two recent volcanic eruptions have provided contradictory evidence on this point.
Mount Agung in 1963 (Indonesia)
apparently caused a considerable decrease in temperatures around much of the world, whereas
El Chichon in 1982 (Mexico),
seemed to have little effect, perhaps because of its different location or because of the El Nino that
occurred the same year. El Nino is a Pacific Ocean phenomenon, but it causes worldwide weather variations
that may have acted to cancel out the effect of the El Chichon eruption.
From:
Myers, et.al., 1997,
What are Volcano Hazards?:
USGS Fact Sheet 002-97
Cataclysmic
eruptions, such as the
June 15, 1991, eruption of Mount Pinatubo
(Philippines), inject huge amounts of sulfur dioxide gas into the
stratosphere, where it combines with water to form an aerosol (mist) of
sulfuric acid. By reflecting solar radiation, such aerosols can lower the
Earth's average surface temperature for extended periods of time by several
degrees Fahrenheit. These sulfuric acid aerosols also contribute to
the destruction of the ozone layer by altering chlorine and nitrogen
compounds in the upper atmosphere.
From:
Self, et.al., 1996,
The Atmospheric Impact of the 1991 Mount Pinatubo Eruption:
IN:
Newhall and Punongbayan, (eds.), 1996,
Fire and Mud: Eruptions and Lahars of Mount Pinatubo, Philippines:
University of Washington Press
As observed after several eruptions, including
Agung in 1963 (Indonesia) and
El Chichon in 1982 (Mexico),
stratospheric warming and lower tropospheric and surface cooling have been documented after the
Pinatubo eruption.
Labitzke and McCormick (1992) show that warming in the lower stratosphere
(16 to 24 kilometers or 30 to 100 mbar) of up to 2 to 3 degrees C occurred within 4 to 5 months
of the eruption between the equator and 20degreesNorth latitude, and it was also later noticed in
middle northern latitudes (Angell, 1993). The warming distribution closely mirrored the dispersal
pattern of the aerosol cloud; this mirroring strongly suggests that the warming was due to absorption
of radiation by the aerosols. The warming was more intense in southern temperate-polar latitudes,
perhaps due to the presence of aerosols from the
Mount Hudson (Chile)
eruption. Such temperature
changes can influence stratospheric dynamics (Pitari, 1992). Since the peak of stratospheric warming
in late 1991, temperatures in the 18- to 24-kilometer region have cooled considerably, passing the
average in early 1993; temperatures in 1993 were the coldest ever recorded (Christy and Drouilhet,
1994; Monastersky, 1994) and may be related to ozone destruction in the lower stratosphere.
Stratospheric temperatures also plummeted and stayed cooler than average for 7 years after the
El Chichon eruption.
Several experiments have measured the radiative climate forcing of the Pinatubo aerosols.
The NASA Earth Radiation Budget Experiment (ERBE) recently
provided the first unambiguous direct measurement of
the climate forcing on a large scale in both hemispheres (Minnis and others, 1993), an average
radiative cooling of 2.7 W/m2 by August 1991. Direct solar beam reductions of 25 to 30
percent were measured at widely distributed stations by Dutton and Christy (1992), while Stowe and
others (1992) showed from AVHRR-derived optical depth measurements that the globally averaged net
radiation at the top of the atmosphere may have decreased by about 2.5 W/m2 in late 1991.
These values translate into a global cooling of at least 0.5 to 0.7 degrees C, as seen in the global
and Northern Hemisphere temperature records by September 1992 (Dutton and Christy, 1992). A net
cooling effect of approximately 0.3 degrees C was estimated as a result of the El Chichon
aerosol (Angell and Korshover, 1983; Handler, 1989), but the overall potential cooling caused by the
El Chichon cloud was moderated by warming assiciated with El-Nino-Southern Oscillation
(Angell, 1988, 1990). Pinatubo had a much larger radiative influence than El Chichon in
the Southern Hemisphere (Dutton and Christy, 1992). Pinatubo's cloud caused about 1.7 times the
global radiative forcing of El Chichon, making the estimated cooling of 0.5 degrees C a more
robust figure.
One possible opposite effect, leading to surface warming, may have been caused by stratospheric to
tropospheric transport of aerosols, due to aerosol-induced changes in atmospheric dynamics, and in a
theoretical study Jensen and Toon (1992) suggest that this process may cause higher than usual amounts
of cirrus clouds in the upper troposphere. Warmer than average winters and cooler than average summers
over continental Northern Hemisphere areas have been documented and modeled after several eruptions,
including Pinatubo, and this appears to be part of the normal Northern Hemisphere response after
volcanic aerosol events (Groisman, 1992; Robock and Liu, 1994).
Volcanic Smog ("Vog") and Acid Rain
From:
Heliker, et.al., 1997,
Living on Active Volcanoes -- The Island of Hawai'i:
USGS Fact Sheet 074-97
Sulfur dioxide gas, continuously emitted during Kilauea's
current long-lived eruption, has resulted in persistent
volcanic smog ("vog") in downwind areas.
Vog, as well as acid rain, forms
when sulfur dioxide reacts with atmospheric moisture. Vog aggravates
respiratory problems, and acid rain damages crops and corrodes metal. On the
Island of Hawai'i, the drinking water of many homes with rain-water catchment
systems has been contaminated by lead leached by acid rain from roofing and
plumbing materials.
From:
Myers, et.al., 1997,
What are Volcano Hazards?:
USGS Fact Sheet 002-97
Volcanoes emit
gases during eruptions.
Even when a volcano is not erupting,
cracks in the ground allow gases to reach the surface through small
openings called fumaroles. Ninety percent of all gas emitted by volcanoes
is water vapor (steam), most of which is heated ground water (underground
water from rain fall and streams). Other common volcanic gases are carbon
dioxide, sulfur dioxide, hydrogen sulfide, hydrogen, and fluorine. Sulfur
dioxide gas can react with water droplets in the atmosphere to create
acid rain,
which causes corrosion and harms vegetation. Carbon dioxide is
heavier than air and can be trapped in low areas in concentrations that are
deadly to people and animals. Fluorine, which in high concentrations is
toxic, can be adsorbed onto volcanic ash particles that later fall to the
ground. The fluorine on the particles can poison livestock grazing on
ash-coated grass and also contaminate domestic water supplies.
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08/02/05, Lyn Topinka