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dc.contributor.authorCanchala, Teresita-
dc.contributor.authorCerón, Wilmar Loaiza-
dc.contributor.authorFrances, Felix-
dc.contributor.authorCarvajal-Escobar, Yesid-
dc.contributor.authorAndreoli, Rita Valéria-
dc.contributor.authorKayano, Mary Toshie-
dc.contributor.authorAlfonso-Morales, Wilfredo-
dc.contributor.authorCaicedo-Bravo, Eduardo-
dc.contributor.authorSouza, Rodrigo Augusto Ferreira de-
dc.date.accessioned2020-05-14T14:27:39Z-
dc.date.available2020-05-14T14:27:39Z-
dc.date.issued2020-
dc.identifier.urihttps://repositorio.inpa.gov.br/handle/1/15456-
dc.description.abstractOceanic-atmospheric phenomena of different time scales concurrently might affect the streamflow in several basins around the world. The Atrato River Basin (ARB) and Patia River Basin (PRB) of the Colombian Pacific region are examples of such basins. Nevertheless, the relations between the streamflows in the ARB and PRB and the oceanic-atmospheric factors have not been examined considering different temporal scales. Hence, this article studies the relations of the climate indices and the variability of the streamflows in the ARB and PRB at interannual and decadal timescales. To this, the streamflow variability modes were obtained from the principal component analysis (PCA); furthermore, their linear dependence with indices of the El Nino/Southern Oscillation (ENSO), precipitation (PRP), the Choco low-level jet (CJ), and other indices were quantified through (a) Pearson and Kendall's tau correlations, and (b) wavelet transform. The PCA presented a single significant mode for each basin, with an explained variance of around 80%. The correlation analyses between the PC1s of the ARB and PRB, and the climate indices showed significant positive (negative) high correlations with PRP, CJ, and Southern Oscillation Index (SOI) (ENSO indices). The wavelet coherence analysis showed significant coherencies between ENSO and ARB: at interannual (2-7 years) and decadal scale (8-14), preferably with the sea surface temperature (SST) in the east and west Tropical Pacific Ocean (TPO). For PRB with the SST in the central and western regions of the TPO in the interannual (4-8 years) and decadal (8-14 years) scales, the decreases (increases) in streamflow precede the El Nino (La Nina) events. These results indicate multiscale relations between the basins' streamflow and climate phenomena not documented in previous works, relevant to forecast the extreme flow events in the Colombian Pacific rivers and for planning and implementing strategies for the sustainable use of water resources in the basins studied. © 2020 by the authors.en
dc.language.isoenpt_BR
dc.relation.ispartofVolume 12, Número 2pt_BR
dc.rightsAttribution-NonCommercial-NoDerivs 3.0 Brazil*
dc.rights.urihttp://creativecommons.org/licenses/by-nc-nd/3.0/br/*
dc.subjectAtmospheric Movementsen
dc.subjectAtmospheric Pressureen
dc.subjectClimatologyen
dc.subjectOceanographyen
dc.subjectRiversen
dc.subjectStream Flowen
dc.subjectWatershedsen
dc.subjectWavelet Analysisen
dc.subjectWavelet Transformsen
dc.subjectAtmospheric Phenomenaen
dc.subjectClimate Indexen
dc.subjectColombiansen
dc.subjectEl Nino/southern Oscillationsen
dc.subjectSea Surface Temperature (sst)en
dc.subjectSouthern Oscillation Indexen
dc.subjectStreamflow Variabilityen
dc.subjectPacific Ocean (tropical)en
dc.subjectPrincipal Component Analysisen
dc.subjectEl Nino-southern Oscillationen
dc.subjectPrincipal Component Analysisen
dc.subjectSea Surface Temperatureen
dc.subjectStream Flowen
dc.subjectSustainabilityen
dc.subjectTeleconnectionen
dc.subjectWater Resourcesen
dc.subjectWavelet Analysisen
dc.subjectAtrato Riveren
dc.subjectChocoen
dc.subjectColombiaen
dc.subjectPacific Oceanen
dc.subjectPacific Ocean (tropical)en
dc.subjectPatia Riveren
dc.titleStreamflow variability in colombian pacific basins and their teleconnections with climate indicesen
dc.typeArtigopt_BR
dc.identifier.doi10.3390/w12020526-
dc.publisher.journalWater (Switzerland)pt_BR
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