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DC Field | Value | Language |
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dc.contributor.author | Jain, Vinit | - |
dc.contributor.author | Pandey, R. P. | - |
dc.contributor.author | Jain, M. K. | - |
dc.contributor.author | Byun, Hi-Ryong | - |
dc.date.accessioned | 2019-09-25T10:12:06Z | - |
dc.date.available | 2019-09-25T10:12:06Z | - |
dc.date.issued | 2015 | - |
dc.identifier.citation | Weather and Climate Extremes | en_US |
dc.identifier.uri | http://117.252.14.250:8080/jspui/handle/123456789/3638 | - |
dc.description.abstract | Drought 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.iso | en | en_US |
dc.publisher | Elsevier | en_US |
dc.subject | Drought | en_US |
dc.subject | Effective drought index | en_US |
dc.subject | Standardized precipitation index | en_US |
dc.subject | Z-score | en_US |
dc.subject | China Z-index | en_US |
dc.subject | Rainfall departure | en_US |
dc.subject | Time step of drought | en_US |
dc.title | Comparison of drought indices for appraisal of drought characteristics in the Ken River Basin | en_US |
dc.type | Article | en_US |
Appears in Collections: | Research papers in International Journals |
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