Influence of the Coupling South Atlantic Convergence Zone-El Niño-Southern Oscillation (SACZ-ENSO) on the projected precipitation changes over the central Andes

dc.contributor.authorSulca Jota, Juan Carlos
dc.contributor.authorRocha, Rosmeri P. da
dc.date.accessioned2021-05-18T17:48:59Z
dc.date.available2021-05-18T17:48:59Z
dc.date.issued2021-05-08
dc.description.abstractThere are no studies related to the influence of the coupling between the South Atlantic Convergence Zone (SACZ) and El Niño-Southern Oscillation (ENSO) pattern variability on future changes in the austral summer (December-February, DJF) precipitation over the central Andes. Therefore, we evaluated the historical simulations (1980–2005) and projections (2070–2099) for the Representative Concentration Pathway 8.5 (RCP 8.5) scenario of 25 global climate models (GCMs) from the Coupled Model Intercomparison Project phase 5 (CMIP5). Moreover, we also consider the Regional Climate Model version 4 (RegCM4) projections nested in three CMIP5 GCMs (GFDL-ESM2M, MPI-ESM-MR, and HadGEM2-ES) under RCP 8.5. We separate the CMIP5 GCMs according to their abilities to simulate the nonlinear characteristics of ENSO and the SACZ for the historical period. We found that only three out of 25 CMIP5 GCMs (hereafter group A) simulate the nonlinear characteristics of ENSO and the SACZ during the historical period. Although most CMIP5 GCM project DJF precipitation decreases over the central Andes, group A project precipitation increases related to the projected increase in deep convection over the central Peruvian Amazon. On the regional scale, only RegGFDL (nested in a group A CMIP5 GCM) projects a statistically significant increase in DJF precipitation (~5–15%) over the northern central Andes and the central Peruvian Amazon. Conversely, all RegCM4 simulations project a decrease in DJF precipitation (~−10%) over the southern central Andes.es_ES
dc.description.peer-reviewPor pareses_ES
dc.formatapplication/pdfes_ES
dc.identifier.citationSulca, J. C. & Rocha, R. P. d. (2021). Influence of the Coupling South Atlantic Convergence Zone-El Niño-Southern Oscillation (SACZ-ENSO) on the projected precipitation changes over the central Andes.==$Climate, 9$==(5),77. https://doi.org/10.3390/cli9050077es_ES
dc.identifier.doihttps://doi.org/10.3390/cli9050077es_ES
dc.identifier.govdocindex-oti2018
dc.identifier.journalClimatees_ES
dc.identifier.urihttp://hdl.handle.net/20.500.12816/4943
dc.language.isoenges_ES
dc.publisherMDPIes_ES
dc.relation.ispartofurn:issn:2225-1154
dc.rightsinfo:eu-repo/semantics/openAccesses_ES
dc.rights.urihttps://creativecommons.org/licences/by/4.0/es_ES
dc.subjectAustral summer precipitationes_ES
dc.subjectCentral Andeses_ES
dc.subjectClimate changees_ES
dc.subjectPrecipitationes_ES
dc.subjectNonlinear ENSO characteristicses_ES
dc.subjectCoupling ENSO-SACZes_ES
dc.subjectCMIP5es_ES
dc.subjectFuture changees_ES
dc.subjectRegCM4es_ES
dc.subject.ocdehttps://purl.org/pe-repo/ocde/ford#1.05.09es_ES
dc.subject.ocdehttps://purl.org/pe-repo/ocde/ford#1.05.10es_ES
dc.titleInfluence of the Coupling South Atlantic Convergence Zone-El Niño-Southern Oscillation (SACZ-ENSO) on the projected precipitation changes over the central Andeses_ES
dc.typeinfo:eu-repo/semantics/articlees_ES

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