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@ARTICLE{Hardelauf:57149,
author = {Hardelauf, H. and Javaux, M. and Herbst, M. and Gottschalk,
S. and Kasteel, R. and Vanderborght, J. and Vereecken, H.},
title = {{PARSWMS}: {A} {P}arallelized {M}odel for {S}imulating
{T}hree-{D}imensional {W}ater {F}low and {S}olute
{T}ransport in {V}ariably {S}aturated {S}oils},
journal = {Vadose zone journal},
volume = {6},
issn = {1539-1663},
address = {Madison, Wis.},
publisher = {SSSA},
reportid = {PreJuSER-57149},
pages = {255 - 259},
year = {2007},
note = {Record converted from VDB: 12.11.2012},
abstract = {Three-dimensional vadose zone models are used more and more
for solving hydrological problems on a broad range of scales
with large amount of nodes. Currently, the problems we can
solve in reasonable computational time may have up to 5 x
10(6) nodes. However, distributed models may need up to
10(10) nodes to properly predict. ow and transport at the
watershed scale. The speed and efficiency of current flow
and transport models therefore need to be improved. The
parallelization of the code is one possible way to decrease
the computational time by distributing a complex large
geometry problem over multiple processors working in
parallel. This is the solution we implemented by developing
PARSWMS, a parallelized version of $SWMS_3D$ (Simunek et
al., 1995). The objective of this technical note is to
describe the PARSWMS model, test its reliability, and show
its performance and efficiency compared with single
processor runs.},
keywords = {J (WoSType)},
cin = {ICG-4 / JARA-ENERGY / JARA-SIM},
ddc = {550},
cid = {I:(DE-Juel1)VDB793 / $I:(DE-82)080011_20140620$ /
I:(DE-Juel1)VDB1045},
pnm = {Terrestrische Umwelt},
pid = {G:(DE-Juel1)FUEK407},
shelfmark = {Environmental Sciences / Soil Science / Water Resources},
typ = {PUB:(DE-HGF)16},
UT = {WOS:000248503000005},
doi = {10.2136/vzj2006.0156},
url = {https://juser.fz-juelich.de/record/57149},
}