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A chronology of El niño events from primary documentary sources in northern Peru

dc.contributor.authorGarcía Herrera, Ricardo Francisco
dc.contributor.authorDíaz, H. F.
dc.contributor.authorGarcía, R. R.
dc.contributor.authorPrieto, M. R.
dc.contributor.authorBarriopedro Cepero, David
dc.contributor.authorMoyano, R.
dc.contributor.authorHernández Martín, Emiliano
dc.date.accessioned2023-06-20T10:40:50Z
dc.date.available2023-06-20T10:40:50Z
dc.date.issued2008-05
dc.description© 2008 American Meteorological Society. This work was supported by a grant from the NOAA Climate Program Office’s Climate Change Data and Detection element. J. Castañeda assisted with document identification activities in the Archivo de la Libertad. G. Fernández and E. González searched supplementary information in the Archivo General de Indias. J. A. García discussed a preliminary version of the manuscript. ONERN supplied meteorological information from northern Peru. Three anonymous reviewers provided helpful comments, which improved the original manuscript.
dc.description.abstractThe authors present a chronology of El Niño (EN) events based on documentary records from northern Peru. The chronology, which covers the period 1550-1900, is constructed mainly from primary sources from the city of Trujillo (Peru), the Archivo General de Indias in Seville (Spain), and the Archivo General de la Nacion in Lima (Peru), supplemented by a reassessment of documentary evidence included in previously published literature. The archive in Trujillo has never been systematically evaluated for information related to the occurrence of El Niño-Southern Oscillation (ENSO). Abundant rainfall and river discharge correlate well with EN events in the area around Trujillo, which is very dry during most other years. Thus, rain and flooding descriptors, together with reports of failure of the local fishery, are the main indicators of EN occurrence that the authors have searched for in the documents. A total of 59 EN years are identified in this work. This chronology is compared with the two main previous documentary EN chronologies and with ENSO indicators derived from proxy data other than documentary sources. Overall, the seventeenth century appears to be the least active EN period, while the 1620s, 1720s, 1810s, and 1870s are the most active decades. The results herein reveal long-term fluctuations in warm ENSO activity that compare reasonably well with low-frequency variability deduced from other proxy data.
dc.description.departmentDepto. de Física de la Tierra y Astrofísica
dc.description.facultyFac. de Ciencias Físicas
dc.description.refereedTRUE
dc.description.sponsorshipNOAA Climate Program Office’s Climate Change Data and Detection element
dc.description.statuspub
dc.eprint.idhttps://eprints.ucm.es/id/eprint/24625
dc.identifier.doi10.1175/2007JCLI1830.1
dc.identifier.issn0894-8755
dc.identifier.officialurlhttp://dx.doi.org/10.1175/2007JCLI1830.1
dc.identifier.relatedurlhttp://journals.ametsoc.org/
dc.identifier.urihttps://hdl.handle.net/20.500.14352/50976
dc.issue.number9
dc.journal.titleJournal of climate
dc.language.isoeng
dc.page.final1962
dc.page.initial1948
dc.publisherAmerican Meteorological Society
dc.rights.accessRightsopen access
dc.subject.cdu52
dc.subject.keywordSouthern-oscillation
dc.subject.keywordVariability
dc.subject.keywordClimate
dc.subject.keywordTeleconnections
dc.subject.keywordCenturies
dc.subject.keywordEvolution
dc.subject.keywordEnso
dc.subject.ucmAstrofísica
dc.subject.ucmAstronomía (Física)
dc.subject.ucmFísica atmosférica
dc.subject.unesco2501 Ciencias de la Atmósfera
dc.titleA chronology of El niño events from primary documentary sources in northern Peru
dc.typejournal article
dc.volume.number21
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