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  5. FALL3D-8.0: a computational model for atmospheric transport and deposition of particles, aerosols and radionuclides. Part I: model physics and numerics
 
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FALL3D-8.0: a computational model for atmospheric transport and deposition of particles, aerosols and radionuclides. Part I: model physics and numerics

Author(s)
Folch, Arnau  
CASE Department, Barcelona Supercomputing Center, Barcelona, Spain  
Mingari, Leonardo  
CASE Department, Barcelona Supercomputing Center, Barcelona, Spain  
Gutierrez, Natalia  
CASE Department, Barcelona Supercomputing Center, Barcelona, Spain  
Hanzich, Mauricio  
CASE Department, Barcelona Supercomputing Center, Barcelona, Spain  
Macedonio, Giovanni  
Istituto Nazionale di Geofisica e Vulcanologia (INGV), Sezione OV, Napoli, Italia  
Costa, Antonio  
Istituto Nazionale di Geofisica e Vulcanologia (INGV), Sezione Bologna, Bologna, Italia  
Language
English
Obiettivo Specifico
5V. Processi eruttivi e post-eruttivi
Status
Published
JCR Journal
JCR Journal
Journal
Geoscientific Model Development  
Issue/vol(year)
3/13 (2020)
Publisher
EGU - Copernicus
Pages (printed)
1431–1458
Date Issued
2020
DOI
10.5194/gmd-13-1431-2020
Last version
https://doi.org/10.5194/gmd-2019-311
URI
https://www.earth-prints.org/handle/2122/13185
Subjects
04.08. Volcanology  
Subjects

Atmospheric transport...

Radionuclides

Abstract
This manuscript presents FALL3D-8.0, the last
version release of an open-source code with 15+ years of
track record and a growing number of users in the vol-
canological and atmospheric communities. The code has
been redesigned and rewritten from scratch in the framework
of the EU Center of Excellence for Exascale in Solid Earth
(ChEESE) in order to overcome legacy issues and allow
for successive optimisations that are already planned in the
preparation of the code towards extreme-scale computing.
However, this baseline version already contains substantial
improvements in terms of model physics, solving algorithms,
and code accuracy and performance. The code, originally
conceived for atmospheric dispersal and deposition of tephra
particles, has been extended to model other types of particles, aerosols and radionuclides. The solving strategy has
also been changed, replacing the former central-differences
scheme for a high-resolution central-upwind scheme derived
from finite volumes, which minimises numerical diffusion
even in presence of sharp concentration gradients and discontinuities. The parallelisation strategy, Input/Output (I/O),
model pre-process workflows and memory management have
also been reconsidered, leading to substantial improvements
on code scalability, efficiency, and overall capability to han-
dle much larger problems. This paper details the FALL3D-8.0
model physics and the numerical implementation of the code.
Type
article
File(s)
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Description
Folch et al., 2019
Size

1.07 MB

Format

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Checksum (MD5)

20ff57c96df3a693d099966780066846

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