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Role of Atmospheric Chemistry in the Climate Impacts of Stratospheric Volcanic InjectionsThe climate impact of a volcanic eruption is known to be dependent on the size, location and timing of the eruption. However, the chemistry and composition of the volcanic plume also control its impact on climate. It is not just sulfur dioxide gas, but also the coincident emissions of water, halogens and ash that influence the radiative and climate forcing of an eruption. Improvements in the capability of models to capture aerosol microphysics, and the inclusion of chemistry and aerosol microphysics modules in Earth system models, allow us to evaluate the interaction of composition and chemistry within volcanic plumes in a new way. These modeling efforts also illustrate the role of water vapor in controlling the chemical evolution, and hence climate impacts, of the plume. A growing realization of the importance of the chemical composition of volcanic plumes is leading to a more sophisticated and realistic representation of volcanic forcing in climate simulations, which in turn aids in reconciling simulations and proxy reconstructions of the climate impacts of past volcanic eruptions. More sophisticated simulations are expected to help, eventually, with predictions of the impact on the Earth system of any future large volcanic eruptions.
Document ID
20160010370
Document Type
Reprint (Version printed in journal)
External Source(s)
Authors
Legrande, Allegra N. (NASA Goddard Inst. for Space Studies New York, NY United States)
Tsigaridis, Kostas (Columbia Univ. New York, NY, United States)
Bauer, Susanne E. (Columbia Univ. New York, NY, United States)
Date Acquired
August 16, 2016
Publication Date
August 8, 2016
Publication Information
Publication: Nature Geoscience
Subject Category
Meteorology and Climatology
Report/Patent Number
GSFC-E-DAA-TN34781
Funding Number(s)
CONTRACT_GRANT: NNX14AB99A
Distribution Limits
Public
Copyright
Other
Keywords
Disrupting
Aerosols
Volcanic eruptions