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@ARTICLE{Montzka:837562,
author = {Montzka, Carsten and Herbst, Michael and Weihermüller,
Lutz and Verhoef, Anne and Vereecken, Harry},
title = {{A} global data set of soil hydraulic properties and
sub-grid variability of soil water retention and
hydraulic conductivity curves},
journal = {Earth system science data},
volume = {9},
number = {2},
issn = {1866-3516},
address = {Katlenburg-Lindau},
publisher = {Copernics Publications},
reportid = {FZJ-2017-06450},
pages = {529 - 543},
year = {2017},
abstract = {Agroecosystem models, regional and global climate models,
and numerical weather prediction models require adequate
parameterization of soil hydraulic properties. These
properties are fundamental for describing and predicting
water and energy exchange processes at the transition zone
between solid earth and atmosphere, and regulate
evapotranspiration, infiltration and runoff generation.
Hydraulic parameters describing the soil water retention
(WRC) and hydraulic conductivity (HCC) curves are typically
derived from soil texture via pedotransfer functions (PTFs).
Resampling of those parameters for specific model grids is
typically performed by different aggregation approaches such
a spatial averaging and the use of dominant textural
properties or soil classes. These aggregation approaches
introduce uncertainty, bias and parameter inconsistencies
throughout spatial scales due to nonlinear relationships
between hydraulic parameters and soil texture. Therefore, we
present a method to scale hydraulic parameters to individual
model grids and provide a global data set that overcomes the
mentioned problems. The approach is based on Miller–Miller
scaling in the relaxed form by Warrick, that fits the
parameters of the WRC through all sub-grid WRCs to provide
an effective parameterization for the grid cell at model
resolution; at the same time it preserves the information of
sub-grid variability of the water retention curve by
deriving local scaling parameters. Based on the Mualem–van
Genuchten approach we also derive the unsaturated hydraulic
conductivity from the water retention functions, thereby
assuming that the local parameters are also valid for this
function. In addition, via the Warrick scaling parameter λ,
information on global sub-grid scaling variance is given
that enables modellers to improve dynamical downscaling of
(regional) climate models or to perturb hydraulic parameters
for model ensemble output generation. The present analysis
is based on the ROSETTA PTF of Schaap et al. (2001) applied
to the SoilGrids1km data set of Hengl et al. (2014). The
example data set is provided at a global resolution of
0.25° at https://doi.org/10.1594/PANGAEA.870605.},
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:000406381600001},
doi = {10.5194/essd-9-529-2017},
url = {https://juser.fz-juelich.de/record/837562},
}