Examining the relationship between intermediate-scale soil moisture and terrestrial evaporation within a semi-arid grassland

Handle URI:
http://hdl.handle.net/10754/620914
Title:
Examining the relationship between intermediate-scale soil moisture and terrestrial evaporation within a semi-arid grassland
Authors:
Jana, Raghavendra B. ( 0000-0001-8113-1990 ) ; Ershadi, Ali; McCabe, Matthew F. ( 0000-0002-1279-5272 )
Abstract:
Interactions between soil moisture and terrestrial evaporation affect water cycle behaviour and responses between the land surface and the atmosphere across scales. With strong heterogeneities at the land surface, the inherent spatial variability in soil moisture makes its representation via point-scale measurements challenging, resulting in scale mismatch when compared to coarser-resolution satellite based soil moisture or evaporation estimates. The Cosmic Ray Neutron Probe (CRNP) was developed to address such issues in the measurement and representation of soil moisture at intermediate scales. Here, we present a study to assess the utility of CRNP soil moisture observations in validating model evaporation estimates. The CRNP soil moisture product from a pasture in the semi-arid central west region of New South Wales, Australia, was compared to evaporation derived from three distinct approaches, including the Priestley–Taylor (PT-JPL), Penman–Monteith (PM-Mu), and Surface Energy Balance System (SEBS) models, driven by forcing data from local meteorological station data and remote sensing retrievals from the Moderate Resolution Imaging Spectroradiometer (MODIS) sensor. Pearson’s correlations, quantile–quantile (Q–Q) plots, and analysis of variance (ANOVA) were used to qualitatively and quantitatively evaluate the temporal distributions of soil moisture and evaporation over the study site. The relationships were examined against nearly 2 years of observation data, as well as for different seasons and for defined periods of analysis. Results highlight that while direct correlations of raw data were not particularly instructive, the Q–Q plots and ANOVA illustrate that the root-zone soil moisture represented by the CRNP measurements and the modelled evaporation estimates reflect similar distributions under most meteorological conditions. The PT-JPL and PM-Mu model estimates performed contrary to expectation when high soil moisture and cold temperatures were present, while SEBS model estimates displayed a disconnect from the soil moisture distribution in summers with long dry spells. Importantly, no single evaporation model matched the statistical distribution of the measured soil moisture for the entire period, highlighting the challenges in effectively capturing evaporative flux response within changing landscapes. One of the outcomes of this work is that the analysis points to the feasibility of using intermediate scale soil moisture measurements to evaluate gridded estimates of evaporation, exploiting the independent, yet physically linked nature of these hydrological variables.
KAUST Department:
Water Desalination and Reuse Centre; Biological and Environmental Sciences and Engineering
Citation:
Jana, R. B., A. Ershadi, and M. F. McCabe (2016), Examining the relationship between intermediate scale soil moisture and terrestrial evaporation within a semi-arid grassland, Hydrology and Earth System Sciences, 20(10), 3987-4004, doi:10.5194/hess- 20-3987-2016.
Publisher:
Copernicus GmbH
Journal:
Hydrology and Earth System Sciences
Issue Date:
30-Sep-2016
DOI:
10.5194/hess-20-3987-2016
Type:
Article
ISSN:
1027-5606
Sponsors:
Research reported in this publication was supported by the King Abdullah University of Science and Technology (KAUST), Saudi Arabia. The CosmOz instrument was supported by the Commonwealth Scientific and Industry Research Organization (CSIRO). Instrumentation at the Baldry site was funded and commissioned as part of the Australian government’s National Collaborative Research Infrastructure Strategy (NCRIS) and the University of New South Wales. Ali Ershadi was supported by the Australian Research Council Discovery Project (DP120104718).
Additional Links:
http://www.hydrol-earth-syst-sci.net/20/3987/2016/
Appears in Collections:
Articles

Full metadata record

DC FieldValue Language
dc.contributor.authorJana, Raghavendra B.en
dc.contributor.authorErshadi, Alien
dc.contributor.authorMcCabe, Matthew F.en
dc.date.accessioned2016-10-11T05:42:15Z-
dc.date.available2016-10-11T05:42:15Z-
dc.date.issued2016-09-30-
dc.identifier.citationJana, R. B., A. Ershadi, and M. F. McCabe (2016), Examining the relationship between intermediate scale soil moisture and terrestrial evaporation within a semi-arid grassland, Hydrology and Earth System Sciences, 20(10), 3987-4004, doi:10.5194/hess- 20-3987-2016.en
dc.identifier.issn1027-5606-
dc.identifier.doi10.5194/hess-20-3987-2016-
dc.identifier.urihttp://hdl.handle.net/10754/620914-
dc.description.abstractInteractions between soil moisture and terrestrial evaporation affect water cycle behaviour and responses between the land surface and the atmosphere across scales. With strong heterogeneities at the land surface, the inherent spatial variability in soil moisture makes its representation via point-scale measurements challenging, resulting in scale mismatch when compared to coarser-resolution satellite based soil moisture or evaporation estimates. The Cosmic Ray Neutron Probe (CRNP) was developed to address such issues in the measurement and representation of soil moisture at intermediate scales. Here, we present a study to assess the utility of CRNP soil moisture observations in validating model evaporation estimates. The CRNP soil moisture product from a pasture in the semi-arid central west region of New South Wales, Australia, was compared to evaporation derived from three distinct approaches, including the Priestley–Taylor (PT-JPL), Penman–Monteith (PM-Mu), and Surface Energy Balance System (SEBS) models, driven by forcing data from local meteorological station data and remote sensing retrievals from the Moderate Resolution Imaging Spectroradiometer (MODIS) sensor. Pearson’s correlations, quantile–quantile (Q–Q) plots, and analysis of variance (ANOVA) were used to qualitatively and quantitatively evaluate the temporal distributions of soil moisture and evaporation over the study site. The relationships were examined against nearly 2 years of observation data, as well as for different seasons and for defined periods of analysis. Results highlight that while direct correlations of raw data were not particularly instructive, the Q–Q plots and ANOVA illustrate that the root-zone soil moisture represented by the CRNP measurements and the modelled evaporation estimates reflect similar distributions under most meteorological conditions. The PT-JPL and PM-Mu model estimates performed contrary to expectation when high soil moisture and cold temperatures were present, while SEBS model estimates displayed a disconnect from the soil moisture distribution in summers with long dry spells. Importantly, no single evaporation model matched the statistical distribution of the measured soil moisture for the entire period, highlighting the challenges in effectively capturing evaporative flux response within changing landscapes. One of the outcomes of this work is that the analysis points to the feasibility of using intermediate scale soil moisture measurements to evaluate gridded estimates of evaporation, exploiting the independent, yet physically linked nature of these hydrological variables.en
dc.description.sponsorshipResearch reported in this publication was supported by the King Abdullah University of Science and Technology (KAUST), Saudi Arabia. The CosmOz instrument was supported by the Commonwealth Scientific and Industry Research Organization (CSIRO). Instrumentation at the Baldry site was funded and commissioned as part of the Australian government’s National Collaborative Research Infrastructure Strategy (NCRIS) and the University of New South Wales. Ali Ershadi was supported by the Australian Research Council Discovery Project (DP120104718).en
dc.language.isoenen
dc.publisherCopernicus GmbHen
dc.relation.urlhttp://www.hydrol-earth-syst-sci.net/20/3987/2016/en
dc.rights© Author(s) 2016. This work is distributed under the Creative Commons Attribution 3.0 License.en
dc.subjectSoil moistureen
dc.subjectland surface evaporationen
dc.subjectCRNPen
dc.subjectSEBSen
dc.subjectPT-JPLen
dc.subjectPm-Muen
dc.titleExamining the relationship between intermediate-scale soil moisture and terrestrial evaporation within a semi-arid grasslanden
dc.typeArticleen
dc.contributor.departmentWater Desalination and Reuse Centreen
dc.contributor.departmentBiological and Environmental Sciences and Engineeringen
dc.identifier.journalHydrology and Earth System Sciencesen
dc.eprint.versionPublisher's Version/PDFen
dc.contributor.affiliationKing Abdullah University of Science and Technology (KAUST)en
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