Please use this identifier to cite or link to this item: http://117.252.14.250:8080/jspui/handle/123456789/3638
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dc.contributor.authorJain, Vinit-
dc.contributor.authorPandey, R. P.-
dc.contributor.authorJain, M. K.-
dc.contributor.authorByun, Hi-Ryong-
dc.date.accessioned2019-09-25T10:12:06Z-
dc.date.available2019-09-25T10:12:06Z-
dc.date.issued2015-
dc.identifier.citationWeather and Climate Extremesen_US
dc.identifier.urihttp://117.252.14.250:8080/jspui/handle/123456789/3638-
dc.description.abstractDrought indicesareusedtomonitordroughtconditionsofaregion.Variousdroughtindices(DIs)have been proposedinpastfewdecades,butsomeofthoseareregionspecific andhavelimitationsofap- plicability inotherclimaticconditions.Also,multipletimestepsofDIsmakeithardtodecidethatwhich time stepisthebesttoshowthedroughtcondition. Present studyaimstocompareStandardizedPrecipitationIndex(SPI),EffectiveDroughtIndex(EDI), statistical Z-Score,China Z-Index(CZI),RainfallDeparture(RD),RainfallDecilebasedDroughtIndex (RDDI) fortheirsuitabilityindroughtpronedistrictsoftheKenRiverBasin,locatedincentralIndia, where therainfallisconcentratedinthemonsoonseason(June–September)andfrequentoccurrenceof severedroughteventsarecommon.AllselectedDIswithmultipletimestepsareappliedtocomputethe severity for five timestepsof1,3,6,9,and12-month,andcomparedwitheachotherandEDI. The studyrevealsthat(1)1-monthtimestepinallDIsmayproduceerroneousestimatesofdrought duration. (2)Thedroughtindicescomputedfor9-monthtimesteparebestcorrelatedwitheachother. However,thedroughtdurationandthedroughtfrequenciesestimatedusingRDandRDDIareindis- agreement withotherDIs,therefore,thesearenotsuitableforthisareawherethesummerconcentration of precipitationisveryhigh.(3)TheDIsarehighlycorrelatedatsametimestepsandcanalternativelybe used. However,theyarepoorlycorrelatedatdissimilartimesteps,whichmakesithardtoassesswhether the droughtoccurredornot.(4)Becausetherearenoobjectiverulestoselecttheappropriatetimestep, and theidentified droughtdurationvariestoomuchwithdifferenttimesteps,itisveryhardagainto assess whenthedroughtoccurred. However,EDI,thathasself-defined timestepinitself,andfreefromtimestepproblem,(1)iscor- relatedbetterwithotherDIsforalltimestepsandeffectiveonlongandshortdroughttogether,with highest correlationat9-monthtimesteps,(2)identifies thedroughtconditionearlierthananyother indices, therefore,(3)isfoundtobemoresuitabledroughtindexforthestudybasin.Thisisinagreement with theresultofEDIapplicationinKorea,Japan,Turkey,AustraliaandIranthoughthemethodsofits testing aredifferent.en_US
dc.language.isoenen_US
dc.publisherElsevieren_US
dc.subjectDroughten_US
dc.subjectEffective drought indexen_US
dc.subjectStandardized precipitation indexen_US
dc.subjectZ-scoreen_US
dc.subjectChina Z-indexen_US
dc.subjectRainfall departureen_US
dc.subjectTime step of droughten_US
dc.titleComparison of drought indices for appraisal of drought characteristics in the Ken River Basinen_US
dc.typeArticleen_US
Appears in Collections:Research papers in International Journals

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