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@ARTICLE{Vereecken:863271,
author = {Vereecken, Harry and Weihermüller, Lutz and Assouline,
Shmuel and Šimůnek, Jirka and Verhoef, Anne and Herbst,
Michael and Archer, Nicole and Mohanty, Binayak and Montzka,
Carsten and Vanderborght, Jan and Balsamo, Gianpaolo and
Bechtold, Michel and Boone, Aaron and Chadburn, Sarah and
Cuntz, Matthias and Decharme, Bertrand and Ducharne, Agnès
and Ek, Michael and Garrigues, Sebastien and Görgen, Klaus
and Ingwersen, Joachim and Kollet, Stefan and Lawrence,
David M. and Li, Qian and Or, Dani and Swenson, Sean and de
Vrese, Philipp and Walko, Robert and Wu, Yihua and Xue,
Yongkang},
title = {{I}nfiltration from the {P}edon to {G}lobal {G}rid
{S}cales: {A}n {O}verview and {O}utlook for {L}and {S}urface
{M}odeling},
journal = {Vadose zone journal},
volume = {18},
number = {1},
issn = {1539-1663},
address = {Alexandria, Va.},
publisher = {GeoScienceWorld},
reportid = {FZJ-2019-03361},
pages = {},
year = {2019},
abstract = {Infiltration in soils is a key process that partitions
precipitation at the land surface into surface runoff and
water that enters the soil profile. We reviewed the basic
principles of water infiltration in soils and we analyzed
approaches commonly used in land surface models (LSMs) to
quantify infiltration as well as its numerical
implementation and sensitivity to model parameters. We
reviewed methods to upscale infiltration from the point to
the field, hillslope, and grid cell scales of LSMs. Despite
the progress that has been made, upscaling of local-scale
infiltration processes to the grid scale used in LSMs is
still far from being treated rigorously. We still lack a
consistent theoretical framework to predict effective fluxes
and parameters that control infiltration in LSMs. Our
analysis shows that there is a large variety of approaches
used to estimate soil hydraulic properties. Novel, highly
resolved soil information at higher resolutions than the
grid scale of LSMs may help in better quantifying subgrid
variability of key infiltration parameters. Currently, only
a few LSMs consider the impact of soil structure on soil
hydraulic properties. Finally, we identified several
processes not yet considered in LSMs that are known to
strongly influence infiltration. Especially, the impact of
soil structure on infiltration requires further research. To
tackle these challenges and integrate current knowledge on
soil processes affecting infiltration processes into LSMs,
we advocate a stronger exchange and scientific interaction
between the soil and the land surface modeling communities.},
cin = {IBG-3},
ddc = {550},
cid = {I:(DE-Juel1)IBG-3-20101118},
pnm = {255 - Terrestrial Systems: From Observation to Prediction
(POF3-255)},
pid = {G:(DE-HGF)POF3-255},
typ = {PUB:(DE-HGF)16},
UT = {WOS:000472523800001},
doi = {10.2136/vzj2018.10.0191},
url = {https://juser.fz-juelich.de/record/863271},
}