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@INPROCEEDINGS{Liu:884299,
author = {Liu, M. and Huang, Y. and Hoffmann, Lars and Huang, C. and
Chen, P. and Heng, Y.},
title = {{H}igh-{R}esolution {S}ource {E}stimation of {V}olcanic
{S}ulfur {D}ioxide {E}missions {U}sing {L}arge-{S}cale
{T}ransport {S}imulations},
volume = {12139},
address = {Cham},
publisher = {Springer},
reportid = {FZJ-2020-03185},
series = {Lecture Notes in Computer Science},
pages = {60-73},
year = {2020},
comment = {Computational Science – ICCS 2020},
booktitle = {Computational Science – ICCS 2020},
abstract = {High-resolution reconstruction of emission rates from
different sources is essential to achieve accurate
simulations of atmospheric transport processes. How to
achieve real-time forecasts of atmospheric transport is
still a great challenge, in particular due to the large
computational demands of this problem. Considering a case
study of volcanic sulfur dioxide emissions, the codes of the
Lagrangian particle dispersion model MPTRAC and an inversion
algorithm for emission rate estimation based on sequential
importance resampling are deployed on the Tianhe-2
supercomputer. The high-throughput based parallel computing
strategy shows excellent scalability and computational
efficiency. Therefore, the spatial-temporal resolution of
the emission reconstruction can be improved by increasing
the parallel scale. In our study, the largest parallel scale
is up to 1.446 million compute processes, which allows us to
obtain emission rates with a resolution of 30 min in time
and 100 m in altitude. By applying massive-parallel
computing systems such as Tianhe-2, real-time source
estimation and forecasts of atmospheric transport are
becoming feasible.},
month = {Jun},
date = {2020-06-03},
organization = {International Conference on
Computational Science 2020, Amsterdam
(The Netherlands), 3 Jun 2020 - 5 Jun
2020},
cin = {JSC},
cid = {I:(DE-Juel1)JSC-20090406},
pnm = {511 - Computational Science and Mathematical Methods
(POF3-511) / DFG project 410579391 - Transportwege für
Aerosol und Spurengase im Asiatischen Monsun in der oberen
Troposphäre und unteren Stratosphäre},
pid = {G:(DE-HGF)POF3-511 / G:(GEPRIS)410579391},
typ = {PUB:(DE-HGF)8 / PUB:(DE-HGF)7},
UT = {WOS:000841756000005},
doi = {10.1007/978-3-030-50420-5_5},
url = {https://juser.fz-juelich.de/record/884299},
}