TY - JOUR
T1 - Pedotransfer Functions in Earth System Science
T2 - Challenges and Perspectives
AU - Van Looy, Kris
AU - Bouma, Johan
AU - Herbst, Michael
AU - Koestel, John
AU - Minasny, Budiman
AU - Mishra, Umakant
AU - Montzka, Carsten
AU - Nemes, Attila
AU - Pachepsky, Yakov A.
AU - Padarian, José
AU - Schaap, Marcel G.
AU - Tóth, Brigitta
AU - Verhoef, Anne
AU - Vanderborght, Jan
AU - van der Ploeg, Martine J.
AU - Weihermüller, Lutz
AU - Zacharias, Steffen
AU - Zhang, Yonggen
AU - Vereecken, Harry
N1 - Funding Information:
A. Nemes acknowledges financial sup port by the FRINATEK program of the Norwegian Research Council (NFR), project 240663, “SoilSpace.” Contributions of U. Mishra were sup ported by a grant from the Office of Science, Office of Biological and Environmental Research of the U.S. Department of Energy under Argonne National Laboratory contract DE-AC02- 06CH11357. B. Tóth is supported by the Hungarian National Research, Development and Innovation Office (NRDI) under grant KH124765. We thank the following people for providing information with regard to the hydraulic and thermal functioning of the various LSMs mentioned in this manuscript: CABLE: Mark Decker; catchment land surface model: Randy Koster, Gabriëlle De Lannoy, and Joe Santanello; CLM: David Lawrence; JSBACH: Stefan Hagemann, with inputs from Christian Beer; JULES: inputs from Imtiaz Dharssi, Toby Marthews, Pier Luigi Vidale, Heather Ashton, and John Edwards; MPI-HM: Tobias Stacke; NOAH-(MP): Yihua Wu and Michel Ek; OLAM: Robert Walko; ORCHIDEE: Agnès Ducharne and Fuxing Wang; SSiB: Yongkang Xue, Qian Li; and SURFEX-ISBA: Aaron Boone and Sebastien Garrigues. The data applied in this paper (Figure 5) with Mualem-Van Genuchten data at continental scale are available at https://doi.pangaea.de/ 10.1594/PANGAEA.870605, and with subgrid soil moisture variability of satellite products: https://doi.pangaea. de/10.1594/PANGAEA.878889.
Publisher Copyright:
©2017. The Authors.
PY - 2017/12
Y1 - 2017/12
N2 - Soil, through its various functions, plays a vital role in the Earth's ecosystems and provides multiple ecosystem services to humanity. Pedotransfer functions (PTFs) are simple to complex knowledge rules that relate available soil information to soil properties and variables that are needed to parameterize soil processes. In this paper, we review the existing PTFs and document the new generation of PTFs developed in the different disciplines of Earth system science. To meet the methodological challenges for a successful application in Earth system modeling, we emphasize that PTF development has to go hand in hand with suitable extrapolation and upscaling techniques such that the PTFs correctly represent the spatial heterogeneity of soils. PTFs should encompass the variability of the estimated soil property or process, in such a way that the estimation of parameters allows for validation and can also confidently provide for extrapolation and upscaling purposes capturing the spatial variation in soils. Most actively pursued recent developments are related to parameterizations of solute transport, heat exchange, soil respiration, and organic carbon content, root density, and vegetation water uptake. Further challenges are to be addressed in parameterization of soil erosivity and land use change impacts at multiple scales. We argue that a comprehensive set of PTFs can be applied throughout a wide range of disciplines of Earth system science, with emphasis on land surface models. Novel sensing techniques provide a true breakthrough for this, yet further improvements are necessary for methods to deal with uncertainty and to validate applications at global scale.
AB - Soil, through its various functions, plays a vital role in the Earth's ecosystems and provides multiple ecosystem services to humanity. Pedotransfer functions (PTFs) are simple to complex knowledge rules that relate available soil information to soil properties and variables that are needed to parameterize soil processes. In this paper, we review the existing PTFs and document the new generation of PTFs developed in the different disciplines of Earth system science. To meet the methodological challenges for a successful application in Earth system modeling, we emphasize that PTF development has to go hand in hand with suitable extrapolation and upscaling techniques such that the PTFs correctly represent the spatial heterogeneity of soils. PTFs should encompass the variability of the estimated soil property or process, in such a way that the estimation of parameters allows for validation and can also confidently provide for extrapolation and upscaling purposes capturing the spatial variation in soils. Most actively pursued recent developments are related to parameterizations of solute transport, heat exchange, soil respiration, and organic carbon content, root density, and vegetation water uptake. Further challenges are to be addressed in parameterization of soil erosivity and land use change impacts at multiple scales. We argue that a comprehensive set of PTFs can be applied throughout a wide range of disciplines of Earth system science, with emphasis on land surface models. Novel sensing techniques provide a true breakthrough for this, yet further improvements are necessary for methods to deal with uncertainty and to validate applications at global scale.
KW - biogeochemical processes
KW - extrapolation
KW - heat flow
KW - hydraulic properties
KW - land surface model
KW - soil properties
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U2 - 10.1002/2017RG000581
DO - 10.1002/2017RG000581
M3 - Review article
AN - SCOPUS:85039167142
SN - 8755-1209
VL - 55
SP - 1199
EP - 1256
JO - Reviews of Geophysics
JF - Reviews of Geophysics
IS - 4
ER -