Modeling influence of soil properties in different gradients of soil moisture: the case of the Valencia Anchor Station Validation Site, Spain
Modeling influence of soil properties in different gradients of soil moisture: the case of the Valencia Anchor Station Validation Site, Spain
The prediction of spatial and temporal variation of soil water content brings numerous benefits in the studies of soil. However, it requires a considerable number of covariates to be included in the study, complicating the analysis. Integrated nested Laplace approximations (INLA) with stochastic partial differential equation (SPDE) methodology is a possible approach that allows the inclusion of covariates in an easy way. The current study has been conducted using INLA-SPDE to study soil moisture in the area of the Valencia Anchor Station (VAS), soil moisture validation site for the European Space Agency SMOS (Soil Moisture and Ocean Salinity). The data used were collected in a typical ecosystem of the semiarid Mediterranean conditions, subdivided into physio-hydrological units (SMOS units) which presents a certain degree of internal uniformity with respect to hydrological parameters and capture the spatial and temporal variation of soil moisture at the local fine scale. The paper advances the knowledge of the influence of hydrodynamic properties on VAS soil moisture (texture, porosity/bulk density and soil organic matter and land use). With the goal of understanding the factors that affect the variability of soil moisture in the SMOS pixel (50 km × 50 km), five states of soil moisture are proposed. We observed that the model with all covariates and spatial effect has the lowest DIC value. In addition, the correlation coefficient was close to 1 for the relationship between observed and predicted values. The methodology applied presents the possibility to analyze the significance of different covariates having spatial and temporal effects. This process is substantially faster and more effective than traditional kriging. The findings of this study demonstrate an advancement in that framework, demonstrating that it is faster than previous methodologies, provides significance of individual covariates, is reproducible, and is easy to compare with models.
Carbó, Ester
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Juan, Pablo
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Añó, Carlos
65467259-4491-4474-8eee-d3491b1e752f
Chaudhuri, Somnath
ae0507e0-f920-4438-bc9f-ecdd5ac8967a
Diaz-Avalos, Carlos
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López-Baeza, Ernesto
24f3c9b8-46ff-4000-b73b-9e6038c00b99
19 December 2021
Carbó, Ester
8cc23850-08ef-478b-8996-c6760b707219
Juan, Pablo
f3648398-5752-4dd0-9410-835566b659f4
Añó, Carlos
65467259-4491-4474-8eee-d3491b1e752f
Chaudhuri, Somnath
ae0507e0-f920-4438-bc9f-ecdd5ac8967a
Diaz-Avalos, Carlos
c3d206d1-9a32-4e8c-88ab-0b7f2cb18e30
López-Baeza, Ernesto
24f3c9b8-46ff-4000-b73b-9e6038c00b99
Carbó, Ester, Juan, Pablo, Añó, Carlos, Chaudhuri, Somnath, Diaz-Avalos, Carlos and López-Baeza, Ernesto
(2021)
Modeling influence of soil properties in different gradients of soil moisture: the case of the Valencia Anchor Station Validation Site, Spain.
Remote Sensing, 13 (24), [5155].
(doi:10.3390/rs13245155).
Abstract
The prediction of spatial and temporal variation of soil water content brings numerous benefits in the studies of soil. However, it requires a considerable number of covariates to be included in the study, complicating the analysis. Integrated nested Laplace approximations (INLA) with stochastic partial differential equation (SPDE) methodology is a possible approach that allows the inclusion of covariates in an easy way. The current study has been conducted using INLA-SPDE to study soil moisture in the area of the Valencia Anchor Station (VAS), soil moisture validation site for the European Space Agency SMOS (Soil Moisture and Ocean Salinity). The data used were collected in a typical ecosystem of the semiarid Mediterranean conditions, subdivided into physio-hydrological units (SMOS units) which presents a certain degree of internal uniformity with respect to hydrological parameters and capture the spatial and temporal variation of soil moisture at the local fine scale. The paper advances the knowledge of the influence of hydrodynamic properties on VAS soil moisture (texture, porosity/bulk density and soil organic matter and land use). With the goal of understanding the factors that affect the variability of soil moisture in the SMOS pixel (50 km × 50 km), five states of soil moisture are proposed. We observed that the model with all covariates and spatial effect has the lowest DIC value. In addition, the correlation coefficient was close to 1 for the relationship between observed and predicted values. The methodology applied presents the possibility to analyze the significance of different covariates having spatial and temporal effects. This process is substantially faster and more effective than traditional kriging. The findings of this study demonstrate an advancement in that framework, demonstrating that it is faster than previous methodologies, provides significance of individual covariates, is reproducible, and is easy to compare with models.
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remotesensing-13-05155-v2
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Accepted/In Press date: 16 December 2021
Published date: 19 December 2021
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Local EPrints ID: 502621
URI: http://eprints.soton.ac.uk/id/eprint/502621
ISSN: 2072-4292
PURE UUID: dcd299bd-8dce-497b-88e7-16de88b57a2a
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Date deposited: 02 Jul 2025 16:32
Last modified: 22 Aug 2025 02:43
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Author:
Ester Carbó
Author:
Pablo Juan
Author:
Carlos Añó
Author:
Somnath Chaudhuri
Author:
Carlos Diaz-Avalos
Author:
Ernesto López-Baeza
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