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@ARTICLE{Cai:907863,
author = {Cai, Zhongyin and Griessbach, Sabine and Hoffmann, Lars},
title = {{I}mproved estimation of volcanic {SO}2 injections from
satellite retrievals and {L}agrangian transport simulations:
the 2019 {R}aikoke eruption},
journal = {Atmospheric chemistry and physics},
volume = {22},
number = {10},
issn = {1680-7316},
address = {Katlenburg-Lindau},
publisher = {EGU},
reportid = {FZJ-2022-02254},
pages = {6787 - 6809},
year = {2022},
abstract = {Monitoring and modeling of volcanic plumes are important
for understanding the impact of volcanic activity on climate
and for practical concerns, such as aviation safety or
public health. Here, we apply the Lagrangian transport model
Massive-Parallel Trajectory Calculations (MPTRAC) to
estimate the SO2 injections into the upper troposphere and
lower stratosphere by the eruption of the Raikoke volcano
(48.29∘ N, 153.25∘ E) in June 2019 and its
subsequent long-range transport and dispersion. First, we
used SO2 retrievals from the AIRS (Atmospheric Infrared
Sounder) and TROPOMI (TROPOspheric Monitoring Instrument)
satellite instruments together with a backward trajectory
approach to estimate the altitude-resolved SO2 injection
time series. Second, we applied a scaling factor to the
initial estimate of the SO2 mass and added an exponential
decay to simulate the time evolution of the total SO2 mass.
By comparing the estimated SO2 mass and the mass from
TROPOMI retrievals, we show that the volcano injected
2.1 ± 0.2 Tg SO2, and the e-folding lifetime of the
SO2 was about 13 to 17 d. The reconstructed SO2 injection
time series are consistent between using the AIRS nighttime
and the TROPOMI daytime products. Further, we compared
forward transport simulations that were initialized by AIRS
and TROPOMI SO2 products with a constant SO2 injection rate.
The results show that the modeled SO2 change, driven by
chemical reactions, captures the SO2 mass variations from
TROPOMI retrievals. In addition, the forward simulations
reproduce the SO2 distributions in the first ∼10 d after
the eruption. However, diffusion in the forward simulations
is too strong to capture the internal structure of the SO2
clouds, which is further quantified in the simulation of the
compact SO2 cloud from late July to early August. Our study
demonstrates the potential of using combined nadir satellite
retrievals and Lagrangian transport simulations to further
improve SO2 time- and height-resolved injection estimates of
volcanic eruptions.},
cin = {JSC},
ddc = {550},
cid = {I:(DE-Juel1)JSC-20090406},
pnm = {5111 - Domain-Specific Simulation Data Life Cycle Labs
(SDLs) and Research Groups (POF4-511) / DFG project
410579391 - Transportwege für Aerosol und Spurengase im
Asiatischen Monsun in der oberen Troposphäre und unteren
Stratosphäre},
pid = {G:(DE-HGF)POF4-5111 / G:(GEPRIS)410579391},
typ = {PUB:(DE-HGF)16},
UT = {WOS:000799874000001},
doi = {10.5194/acp-22-6787-2022},
url = {https://juser.fz-juelich.de/record/907863},
}