V32A:
Twenty-Five Years of Science from the 1991 Mount Pinatubo Volcano Eruption I
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V32A:
Twenty-Five Years of Science from the 1991 Mount Pinatubo Volcano Eruption I
Twenty-Five Years of Science from the 1991 Mount Pinatubo Volcano Eruption I
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Session ID#: 18210
Session Description:
The 1991 eruption of Pinatubo Volcano in the Philippines was one of the
largest volcanic eruptions of the 20th Century and spawned research in
many disciplines.For example, in the 25 years since the eruption,
volcanologists substantially improved understanding of how strain,
magmatic gases, and groundwater produce the distinctive patterns of
unrest that foretold Pinatubo’s eruption.Atmospheric scientists
discovered that winter warming (a forced positive mode of the Arctic
Oscillation) follows large, sulfate-rich tropical explosive eruptions,
that volcanic eruptions increase the probability of an El Niño in the
following year and affect the Atlantic Multidecadal Oscillation, and
they have quantified the effects of volcanic aerosols on ozone
depletion.On its 25th anniversary, we invite papers that emphasize new
insights arising from the Pinatubo eruption and its aftermath, in
volcanology, volcano-seismology, geochemistry, fluvial and watershed
processes, plume transport, effects on ozone, radiative forcing, and
climate response.
largest volcanic eruptions of the 20th Century and spawned research in
many disciplines.For example, in the 25 years since the eruption,
volcanologists substantially improved understanding of how strain,
magmatic gases, and groundwater produce the distinctive patterns of
unrest that foretold Pinatubo’s eruption.Atmospheric scientists
discovered that winter warming (a forced positive mode of the Arctic
Oscillation) follows large, sulfate-rich tropical explosive eruptions,
that volcanic eruptions increase the probability of an El Niño in the
following year and affect the Atlantic Multidecadal Oscillation, and
they have quantified the effects of volcanic aerosols on ozone
depletion.On its 25th anniversary, we invite papers that emphasize new
insights arising from the Pinatubo eruption and its aftermath, in
volcanology, volcano-seismology, geochemistry, fluvial and watershed
processes, plume transport, effects on ozone, radiative forcing, and
climate response.
Primary Convener: Alan Robock, Rutgers University, Department of Environmental Sciences, New Brunswick, United States
Conveners: Christopher G Newhall, Mirisbiris Garden and Nature Center, Albay, Philippines, Florian Max M Schwandner, Jet Propulsion Laboratory, Pasadena, CA, United States and Allegra N. LeGrande, NASA Goddard Institute for Space Studies, New York, NY, United States
Chairs: Florian Max M Schwandner, Jet Propulsion Laboratory, Pasadena, CA, United States and Alan Robock, Rutgers University, Department of Environmental Sciences, New Brunswick, United States
OSPA Liaison: Alan Robock, Rutgers University, Department of Environmental Sciences, New Brunswick, United States
Cross-Listed:
- A - Atmospheric Sciences
- GC - Global Environmental Change
Index Terms:
1616 Climate variability [GLOBAL CHANGE]
8408 Volcano/climate interactions [VOLCANOLOGY]
8428 Explosive volcanism [VOLCANOLOGY]
8488 Volcanic hazards and risks [VOLCANOLOGY]
Abstracts Submitted to this Session:
Modern Day Re-analysis of Pinatubo SO2 Injection, Cloud dispersion and Stratospheric Aerosols (129100)
Hydrological sensitivity of volcanically disturbed watersheds—a lesson reinforced at Pinatubo (142858)
See more of: Volcanology, Geochemistry and Petrology
