6533b859fe1ef96bd12b81b1
RESEARCH PRODUCT
Evapotranspiration simulations in ISIMIP2a-Evaluation of spatio-temporal characteristics with a comprehensive ensemble of independent datasets
Wim ThieryDelphine DeryngAkihiko ItoPhilippe CiaisJinfeng ChangJinfeng ChangGuoyong LengYadu PokhrelRene OrthRene OrthSimon N. GoslingJoshua ElliottXingcai LiuThomas HicklerHyungjun KimYusuke SatohNikolay KhabarovChristian FolberthHong YangTian ZhouSonia I. SeneviratneGraham P. WeedonThomas A. M. PughThomas A. M. PughJoerg SteinkampYoshihide WadaMartin HirschiJunguo LiuJunguo LiuLukas GudmundssonYoshimitsu MasakiCatherine MorfopoulosAlexandra-jane HenrotChristoph MüllerRichard WartenburgerTobias StackeErwin SchmidKazuya NishinaXuhui WangSibyll SchaphoffQiuhong TangJustin SheffieldJustin SheffieldHannes Müller Schmiedsubject
PARAMETERIZATION010504 meteorology & atmospheric sciences0208 environmental biotechnologyREANALYSIS DATA02 engineering and technologyForcing (mathematics)01 natural sciencesISIMIP2aEnvironmental Science(all)Evapotranspirationddc:550Range (statistics)Cluster AnalysisMeteorology & Atmospheric SciencesWATERWater cycleuncertaintyGeneral Environmental ScienceUncertaintyVariance (accounting)Explained variationGLOBAL TERRESTRIAL EVAPOTRANSPIRATIONVariable (computer science)[SDU.STU.CL]Sciences of the Universe [physics]/Earth Sciences/ClimatologyClimatologyPhysical SciencesLife Sciences & BiomedicinePROJECTHYDROLOGICAL MODELSevapotranspirationClimate changeEnvironmental Sciences & EcologySOIL-MOISTUREhydrological extreme eventsLAND-SURFACE MODELhydrological extreme events ; cluster analysis ; uncertainty ; ISIMIP2a ; evapotranspiration[SDU.STU.HY]Sciences of the Universe [physics]/Earth Sciences/HydrologyHydrological extreme events0105 earth and related environmental sciencesScience & TechnologyRenewable Energy Sustainability and the EnvironmentPublic Health Environmental and Occupational HealthPOTENTIAL EVAPOTRANSPIRATION020801 environmental engineeringEarth sciencesISIMIP2a; evapotranspiration; uncertainty; cluster analysis; hydrological extreme events13. Climate actionEnvironmental scienceEnvironmental SciencesHIGH-RESOLUTIONcluster analysisdescription
Actual land evapotranspiration (ET) is a key component of the global hydrological cycle and anessential variable determining the evolution of hydrological extreme events under different climate change scenarios. However, recently available ET products show persistent uncertainties thatare impeding a precise attribution of human-induced climate change. Here, we aim at comparing arange of independent global monthly land ET estimates with historical model simulations from theglobal water, agriculture, and biomes sectors participating in the second phase of the Inter-SectoralImpact Model Intercomparison Project (ISIMIP2a). Among the independent estimates, we use theEartH2Observe Tier-1 dataset (E2O), two commonly used reanalyses, a pre-compiled ensembleproduct (LandFlux-EVAL), and an updated collection of recently published datasets thatalgorithmically derive ET from observations or observations-based estimates (diagnostic datasets). Acluster analysis is applied in order to identify spatio-temporal differences among all datasets and tothus identify factors that dominate overall uncertainties. The clustering is controlled by several factorsincluding the model choice, the meteorological forcing used to drive the assessed models, the datacategory (models participating in the different sectors of ISIMIP2a, E2O models, diagnostic estimates,reanalysis-based estimates or composite products), the ET scheme, and the number of soil layers inthe models. By using these factors to explain spatial and spatio-temporal variabilities in ET, we findthat themodel choicemostly dominates (24%–40%of variance explained), except for spatio-temporalpatterns of total ET, where the forcing explains the largest fraction of the variance (29%). The mostdominant clusters of datasets are further compared with individual diagnostic and reanalysis-basedestimates to assess their representation of selected heat waves and droughts in the Great Plains,Central Europe and western Russia. Although most of the ET estimates capture these extreme events,the generally large spread among the entire ensemble indicates substantial uncertainties.
year | journal | country | edition | language |
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2018-06-21 |