Dendrochronological studies in the Peruvian north coast relate to ENSO

dc.contributor.authorRodríguez, R.
dc.contributor.authorMabres, A.
dc.contributor.authorFlores, L.A.
dc.contributor.authorWoodman Pollitt, Ronald Francisco
dc.date.accessioned2016-10-14T15:37:47Z
dc.date.accessioned2017-12-21T19:41:55Z
dc.date.available2016-10-14T15:37:47Z
dc.date.available2017-12-21T19:41:55Z
dc.date.issued2000
dc.description.abstractDendrochronological studies in the peruvian nort coast to find records of past El Niño - Southern Oscillation (ENSO) events began an the ale 80's. The peruvian north coast is the west-most area of South America, close to equator (05o S 80o W) and to the Sechura desert, is a very sensitive area to the climatic changes due to ENSO. An initial selection of several regional trees have been done for study. The study includes phenological observations and tree ring characteristics analysis as well as racial growth control of tree trunks and branches. The species more intensively studied and suitable to fina records due to the ENSO are Palo Santo, Hualtaco and Sapote.es_ES
dc.formatapplication/pdfes_ES
dc.identifier.urihttp://hdl.handle.net/20.500.12816/665
dc.language.isoenges_ES
dc.publisherInstituto Geofísico del Perúes_ES
dc.rightsinfo:eu-repo/semantics/openAccesses_ES
dc.rights.urihttps://creativecommons.org/licences/by/4.0/es_ES
dc.subjectEl Niñoes_ES
dc.subjectClimate changees_ES
dc.subjectAtmospheric precipitationes_ES
dc.subject.ocdehttp://purl.org/pe-repo/ocde/ford#1.05.09es_ES
dc.titleDendrochronological studies in the Peruvian north coast relate to ENSOes_ES
dc.typeinfo:eu-repo/semantics/conferenceObjectes_ES

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