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Monthly and Seasonal Drought Characterization Using GRACE-Based Groundwater Drought Index and Its Link to Teleconnections across South Indian River Basins

dc.contributor.authorSatish Kumar, Kuruvaen
dc.contributor.authorAnandRaj, Pallakuryen
dc.contributor.authorSreelatha, Koppalaen
dc.contributor.authorBisht, Deepak Singhen
dc.contributor.authorSridhar, Venkataramanaen
dc.contributor.departmentBiological Systems Engineeringen
dc.date.accessioned2021-04-09T19:44:01Zen
dc.date.available2021-04-09T19:44:01Zen
dc.date.issued2021-04-03en
dc.date.updated2021-04-09T13:48:37Zen
dc.description.abstractTraditional drought monitoring is based on observed data from both meteorological and hydrological stations. Due to the scarcity of station observation data, it is difficult to obtain accurate drought distribution characteristics, and also tedious to replicate the large-scale information of drought. Thus, Gravity Recovery and Climate Experiment (GRACE) data are utilized in monitoring and characterizing regional droughts where ground station data is limited. In this study, we analyzed and assessed the drought characteristics utilizing the GRACE Groundwater Drought Index (GGDI) over four major river basins in India during the period of 2003–2016. The spatial distribution, temporal evolution of drought, and trend characteristics were analyzed using GGDI. Then, the relationship between GGDI and climate factors were evaluated by the method of wavelet coherence. The results indicate the following points: GRACE’s quantitative results were consistent and robust for drought assessment; out of the four basins, severe drought was noticed in the Cauvery river basin between 2012 and 2015, with severity of −27 and duration of 42 months; other than Godavari river basin, the remaining three basins displayed significant negative trends at monthly and seasonal scales; the wavelet coherence method revealed that climate factors had a substantial effect on GGDI, and the impact of Southern Oscillation Index (SOI) on drought was significantly high, followed by Sea Surface Temperature (SST) Index (namely, NINO3.4) and Multivariate El Niño–Southern Oscillation Index (MEI) in all the basins. This study provides reliable and robust quantitative result of GRACE water storage variations that shares new insights for further drought investigation.en
dc.description.versionPublished versionen
dc.format.mimetypeapplication/pdfen
dc.identifier.citationSatish Kumar, K.; AnandRaj, P.; Sreelatha, K.; Bisht, D.S.; Sridhar, V. Monthly and Seasonal Drought Characterization Using GRACE-Based Groundwater Drought Index and Its Link to Teleconnections across South Indian River Basins. Climate 2021, 9, 56.en
dc.identifier.doihttps://doi.org/10.3390/cli9040056en
dc.identifier.urihttp://hdl.handle.net/10919/102999en
dc.language.isoenen
dc.publisherMDPIen
dc.rightsCreative Commons Attribution 4.0 Internationalen
dc.rights.urihttp://creativecommons.org/licenses/by/4.0/en
dc.subjectGRACEen
dc.subjectGGDIen
dc.subjectdroughten
dc.subjectwavelet coherenceen
dc.subjectteleconnectionsen
dc.titleMonthly and Seasonal Drought Characterization Using GRACE-Based Groundwater Drought Index and Its Link to Teleconnections across South Indian River Basinsen
dc.title.serialClimateen
dc.typeArticle - Refereeden
dc.type.dcmitypeTexten
dc.type.dcmitypeStillImageen

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