Improving soil moisture prediction of a high-resolution land surface model by parameterising pedotransfer functions through assimilation of SMAP satellite data

<p>Pedotransfer functions are used to relate gridded databases of soil texture information to the soil hydraulic and thermal parameters of land surface models. The parameters within these pedotransfer functions are uncertain and calibrated through analyses of point soil samples. How these cali...

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Main Authors: E. Pinnington, J. Amezcua, E. Cooper, S. Dadson, R. Ellis, J. Peng, E. Robinson, R. Morrison, S. Osborne, T. Quaife
Format: Article
Language:English
Published: Copernicus Publications 2021-03-01
Series:Hydrology and Earth System Sciences
Online Access:https://hess.copernicus.org/articles/25/1617/2021/hess-25-1617-2021.pdf
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spelling doaj-a240f91604944e20bd26a4951c3a8f192021-03-31T09:15:05ZengCopernicus PublicationsHydrology and Earth System Sciences1027-56061607-79382021-03-01251617164110.5194/hess-25-1617-2021Improving soil moisture prediction of a high-resolution land surface model by parameterising pedotransfer functions through assimilation of SMAP satellite dataE. Pinnington0J. Amezcua1E. Cooper2S. Dadson3S. Dadson4R. Ellis5J. Peng6J. Peng7E. Robinson8R. Morrison9S. Osborne10T. Quaife11National Centre for Earth Observation, Department of Meteorology, University of Reading, Reading, UKNational Centre for Earth Observation, Department of Meteorology, University of Reading, Reading, UKUK Centre for Ecology and Hydrology, Wallingford, UKUK Centre for Ecology and Hydrology, Wallingford, UKSchool of Geography and the Environment, University of Oxford, Oxford, UKUK Centre for Ecology and Hydrology, Wallingford, UKDepartment of Remote Sensing, Helmholtz Centre for Environmental Research – UFZ, Permoserstraße 15, 04318 Leipzig, GermanyRemote Sensing Centre for Earth System Research, Leipzig University, 04103 Leipzig, GermanyUK Centre for Ecology and Hydrology, Wallingford, UKUK Centre for Ecology and Hydrology, Wallingford, UKMet Office Field Site, Cardington Airfield, Shortstown, Bedford, UKNational Centre for Earth Observation, Department of Meteorology, University of Reading, Reading, UK<p>Pedotransfer functions are used to relate gridded databases of soil texture information to the soil hydraulic and thermal parameters of land surface models. The parameters within these pedotransfer functions are uncertain and calibrated through analyses of point soil samples. How these calibrations relate to the soil parameters at the spatial scale of modern land surface models is unclear because gridded databases of soil texture represent an area average. We present a novel approach for calibrating such pedotransfer functions to improve land surface model soil moisture prediction by using observations from the Soil Moisture Active Passive (SMAP) satellite mission within a data assimilation framework. Unlike traditional calibration procedures, data assimilation always takes into account the relative uncertainties given to both model and observed estimates to find a maximum likelihood estimate. After performing the calibration procedure, we find improved estimates of soil moisture and heat flux for the Joint UK Land Environment Simulator (JULES) land surface model (run at a 1 km resolution) when compared to estimates from a cosmic-ray soil moisture monitoring network (COSMOS-UK) and three flux tower sites. The spatial resolution of the COSMOS probes is much more representative of the 1 km model grid than traditional point-based soil moisture sensors. For 11 cosmic-ray neutron soil moisture probes located across the modelled domain, we find an average 22 % reduction in root mean squared error, a 16 % reduction in unbiased root mean squared error and a 16 % increase in correlation after using data assimilation techniques to retrieve new pedotransfer function parameters.</p>https://hess.copernicus.org/articles/25/1617/2021/hess-25-1617-2021.pdf
collection DOAJ
language English
format Article
sources DOAJ
author E. Pinnington
J. Amezcua
E. Cooper
S. Dadson
S. Dadson
R. Ellis
J. Peng
J. Peng
E. Robinson
R. Morrison
S. Osborne
T. Quaife
spellingShingle E. Pinnington
J. Amezcua
E. Cooper
S. Dadson
S. Dadson
R. Ellis
J. Peng
J. Peng
E. Robinson
R. Morrison
S. Osborne
T. Quaife
Improving soil moisture prediction of a high-resolution land surface model by parameterising pedotransfer functions through assimilation of SMAP satellite data
Hydrology and Earth System Sciences
author_facet E. Pinnington
J. Amezcua
E. Cooper
S. Dadson
S. Dadson
R. Ellis
J. Peng
J. Peng
E. Robinson
R. Morrison
S. Osborne
T. Quaife
author_sort E. Pinnington
title Improving soil moisture prediction of a high-resolution land surface model by parameterising pedotransfer functions through assimilation of SMAP satellite data
title_short Improving soil moisture prediction of a high-resolution land surface model by parameterising pedotransfer functions through assimilation of SMAP satellite data
title_full Improving soil moisture prediction of a high-resolution land surface model by parameterising pedotransfer functions through assimilation of SMAP satellite data
title_fullStr Improving soil moisture prediction of a high-resolution land surface model by parameterising pedotransfer functions through assimilation of SMAP satellite data
title_full_unstemmed Improving soil moisture prediction of a high-resolution land surface model by parameterising pedotransfer functions through assimilation of SMAP satellite data
title_sort improving soil moisture prediction of a high-resolution land surface model by parameterising pedotransfer functions through assimilation of smap satellite data
publisher Copernicus Publications
series Hydrology and Earth System Sciences
issn 1027-5606
1607-7938
publishDate 2021-03-01
description <p>Pedotransfer functions are used to relate gridded databases of soil texture information to the soil hydraulic and thermal parameters of land surface models. The parameters within these pedotransfer functions are uncertain and calibrated through analyses of point soil samples. How these calibrations relate to the soil parameters at the spatial scale of modern land surface models is unclear because gridded databases of soil texture represent an area average. We present a novel approach for calibrating such pedotransfer functions to improve land surface model soil moisture prediction by using observations from the Soil Moisture Active Passive (SMAP) satellite mission within a data assimilation framework. Unlike traditional calibration procedures, data assimilation always takes into account the relative uncertainties given to both model and observed estimates to find a maximum likelihood estimate. After performing the calibration procedure, we find improved estimates of soil moisture and heat flux for the Joint UK Land Environment Simulator (JULES) land surface model (run at a 1 km resolution) when compared to estimates from a cosmic-ray soil moisture monitoring network (COSMOS-UK) and three flux tower sites. The spatial resolution of the COSMOS probes is much more representative of the 1 km model grid than traditional point-based soil moisture sensors. For 11 cosmic-ray neutron soil moisture probes located across the modelled domain, we find an average 22 % reduction in root mean squared error, a 16 % reduction in unbiased root mean squared error and a 16 % increase in correlation after using data assimilation techniques to retrieve new pedotransfer function parameters.</p>
url https://hess.copernicus.org/articles/25/1617/2021/hess-25-1617-2021.pdf
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