https://agupubs.onlinelibrary.wiley.com/doi/full/10.1029/2020JD033578

Unknown Eruption Source Parameters Cause Large Uncertainty in Historical
Volcanic Radiative Forcing Reconstructions

Lauren R. Marshall, Anja Schmidt, Jill S. Johnson, Graham W. Mann, Lindsay
A. Lee, Richard Rigby, Ken S. Carslaw

Abstract

Reconstructions of volcanic aerosol radiative forcing are required to
understand past climate variability. Currently, reconstructions of pre-20th
century volcanic forcing are derived from sulfate concentrations measured
in polar ice cores, mainly using a relationship between the average
ice-sheet sulfate deposition and stratospheric sulfate aerosol burden based
on a single explosive eruption—the 1991 eruption of Mt. Pinatubo. Here we
estimate volcanic radiative forcings and associated uncertainty ranges from
ice-core sulfate records of eight of the largest bipolar deposition signals
in the last 2,500 years using statistical emulation of a perturbed
parameter ensemble of aerosol-climate model simulations of explosive
eruptions. Extensive sampling of different combinations of eruption source
parameters using the emulators reveals that a very wide range of eruptions
in different seasons with different sulfur dioxide emissions, eruption
latitudes, and emission altitudes produce ice-sheet sulfate deposition
consistent with ice-core records. Consequently, we find a large range in
the volcanic forcing that can be directly attributed to the unknown
eruption source parameters. We estimate that the uncertainty in volcanic
forcing caused by many plausible eruption realizations leads to
uncertainties in the global mean surface cooling of around 1°C for the
largest unidentified historical eruptions. Our emulators are available
online (https://cemac.github.io/volcanic-forcing-deposition) where eruption
realizations for given ice-sheet sulfate depositions can be explored.

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