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dc.contributor.authorMueller, B.
dc.contributor.authorHirschi, M.
dc.contributor.authorJimenez, C.
dc.contributor.authorCiais, P.
dc.contributor.authorDirmeyer, P.A.
dc.contributor.authorDolman, A.J.
dc.contributor.authorFisher, J.B.
dc.contributor.authorJung, M.
dc.contributor.authorLudwig, F.
dc.contributor.authorMaignan, F.
dc.contributor.authorMiralles, D.G.
dc.contributor.authorMcCabe, Matthew
dc.contributor.authorReichstein, M.
dc.contributor.authorSheffield, J.
dc.contributor.authorWang, K.
dc.contributor.authorWood, E.F.
dc.contributor.authorZhang, Y.
dc.contributor.authorSeneviratne, S.I.
dc.date.accessioned2014-11-11T14:28:10Z
dc.date.available2014-11-11T14:28:10Z
dc.date.issued2013-10-01
dc.identifier.citationMueller B, Hirschi M, Jimenez C, Ciais P, Dirmeyer PA, et al. (2013) Benchmark products for land evapotranspiration: LandFlux-EVAL multi-data set synthesis. Hydrol Earth Syst Sci 17: 3707-3720. doi:10.5194/hess-17-3707-2013.
dc.identifier.issn10275606
dc.identifier.doi10.5194/hess-17-3707-2013
dc.identifier.urihttp://hdl.handle.net/10754/334520
dc.description.abstractLand evapotranspiration (ET) estimates are available from several global data sets.Here, Monthly Global Land et Synthesis Products, Merged from These Individual Data Sets over the Time Periods 1989-1995 (7 Yr) and 1989-2005 (17 Yr), Are Presented. the Merged Synthesis Products over the Shorter Period Are Based on A Total of 40 Distinct Data Sets while Those over the Longer Period Are Based on A Total of 14 Data Sets. in the Individual Data Sets, et Is Derived from Satellite And/or in Situ Observations (Diagnostic Data Sets) or Calculated Via Land-surface Models (LSMs) Driven with Observations-based Forcing or Output from Atmospheric Reanalyses. Statistics for Four Merged Synthesis Products Are Provided, One Including All Data Sets and Three Including only Data Sets from One Category Each (Diagnostic, LSMs, and Reanalyses). the Multi-annual Variations of et in the Merged Synthesis Products Display Realistic Responses. They Are Also Consistent with Previous Findings of A Global Increase in et between 1989 and 1997 (0.13 Mm yr-2 in Our Merged Product) Followed by A Significant Decrease in This Trend (-0.18 Mm yr-2), although These Trends Are Relatively Small Compared to the Uncertainty of Absolute et Values. the Global Mean et from the Merged Synthesis Products (Based on All Data Sets) Is 493 Mm yr-1 (1.35 Mm d-1) for Both the 1989-1995 and 1989-2005 Products, Which Is Relatively Low Compared to Previously Published Estimates. We Estimate Global Runoff (Precipitation Minus ET) to 263 Mm yr -1 (34 406 km3 yr-1) for A Total Land Area of 130 922 000 km2. Precipitation, Being An Important Driving Factor and Input to Most Simulated et Data Sets, Presents Uncertainties between Single Data Sets As Large As Those in the et Estimates. in Order to Reduce Uncertainties in Current et Products, Improving the Accuracy of the Input Variables, Especially Precipitation, As Well As the Parameterizations of ET, Are Crucial. 2013 Author(s).
dc.language.isoen
dc.publisherCopernicus GmbH
dc.rights.urihttp://creativecommons.org/licenses/by/3.0/
dc.subjectDriving factors
dc.subjectGlobal data
dc.subjectIn-situ observations
dc.subjectInput variables
dc.subjectLand areas
dc.subjectLand surface models
dc.subjectTime-periods
dc.subjectEstimation
dc.subjectEvapotranspiration
dc.subjectUncertainty analysis
dc.subjectWater supply
dc.subjectDiagnostic products
dc.subjectaccuracy assessment
dc.subjectannual variation
dc.subjectdata set
dc.subjectevapotranspiration
dc.subjectprecipitation (climatology)
dc.subjectrunoff
dc.subjectsatellite data
dc.subjectsatellite imagery
dc.titleBenchmark products for land evapotranspiration: LandFlux-EVAL multi-data set synthesis
dc.typeArticle
dc.contributor.departmentBiological and Environmental Sciences and Engineering (BESE) Division
dc.contributor.departmentEarth System Observation and Modelling
dc.contributor.departmentEnvironmental Science and Engineering Program
dc.contributor.departmentWater Desalination and Reuse Research Center (WDRC)
dc.identifier.journalHydrology and Earth System Sciences
dc.eprint.versionPublisher's Version/PDF
dc.contributor.institutionInstitute for Atmospheric and Climate Science, ETH Zurich, Zurich, Switzerland
dc.contributor.institutionLERMA, Observatoire de Paris, Paris, France
dc.contributor.institutionLSCE, UMR CEA, CNRS, Gif-sur-Yvette, France
dc.contributor.institutionGeorge Mason University, Fairfax, VA, United States
dc.contributor.institutionVU University Amsterdam, Netherlands
dc.contributor.institutionJet Propulsion Laboratory, California Institute of Technology, Pasadena, CA, United States
dc.contributor.institutionMax Planck Institute for Biogeochemistry, Jena, Germany
dc.contributor.institutionWageningen University, Wageningen, Netherlands
dc.contributor.institutionSchool of Geographical Sciences, University of Bristol, United Kingdom
dc.contributor.institutionDepartment of Civil and Environmental Engineering, Princeton University, Princeton, NJ, United States
dc.contributor.institutionCollege of Global Change and Earth System Science, Beijing Normal University, Beijing, China
dc.contributor.institutionCSIRO Land and Water, Canberra, Australia
dc.contributor.affiliationKing Abdullah University of Science and Technology (KAUST)
kaust.personMcCabe, Matthew
refterms.dateFOA2018-06-13T15:40:58Z


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