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dc.contributor.author Apaéstegui Campos, James Emiliano
dc.contributor.author Cruz, F. W.
dc.contributor.author Sifeddine, A.
dc.contributor.author Espinoza, Jhan Carlo
dc.contributor.author Guyot, J. L.
dc.contributor.author Khodri, M.
dc.contributor.author Strikis, N.
dc.contributor.author Santos, R. V.
dc.contributor.author Cheng, H.
dc.contributor.author Edwards, L.
dc.contributor.author Carvalho, E.
dc.contributor.author Santini, W.
dc.date.accessioned 2018-09-12T14:44:43Z
dc.date.available 2018-09-12T14:44:43Z
dc.date.issued 2014-02
dc.identifier.citation Apaéstegui, J. E., Cruz, F. W., Sifeddine, A., Espinoza, J. C., Guyot, J. L., Khodri, M., ... & Santini, W. (2014). Hydroclimate variability of the South American Monsoon System during the last 1600 yr inferred from speleothem isotope records of the north-eastern Andes foothills in Peru.==$Climate of the Past Discussions, 10,$==533–561. https://doi:10.5194/cpd-10-533-2014
dc.identifier.govdoc index-oti2018 (NB)
dc.identifier.issn 18149359
dc.identifier.uri http://repositorio.igp.gob.pe/handle/IGP/2938
dc.description.abstract "In this paper we explore a speleothem δ 18O record from Palestina Cave, North Eastern Peru, at a site on the eastern side of the Andes cordillera, upper Amazon Basin, interpreted as a proxy for South America Summer Monsoon (SASM) intensity. This record 5 allows reconstructing SASM activity with ∼ 5 yr time resolution over the last 1600 yr, spanning two major periods of climate variability: the Medieval Climate Anomaly (MCA; 900–1200 AD) and Little Ice Age (LIA 1400–1850 AD) recognized as periods of decrease and increase SASM activity respectively. Time series and wavelet analyses reveal decadal to multidecadal frequencies. Our results suggest that Atlantic Multi10 decadal Oscillation mode (AMO) plays an important role for SASM modulation on multidecadal scale (∼ 65 yr), especially over dry periods such as observed during MCA. Frequencies of 8 and 25 yr simultaneously with multidecadal signal (65 yr) are found over the LIA. and suggest that those modes could be related to North Atlantic Oscillation (NAO) and Interdecadal Pacific Oscillation mode (IPO). Comparison with other 15 South American Paleoprecipitation records shows that the Atlantic and Pacific decadal to multidecadal variability and their teleconnections play an important role in the intensity and the regional patterns of rainfall distribution during the last 1600 yr." es_ES
dc.format application/pdf es_ES
dc.language.iso eng es_ES
dc.publisher European Geosciences Union (EGU) es_ES
dc.rights info:eu-repo/semantics/openAccess es_ES
dc.rights.uri http://creativecommons.org/licences/by-nc-nd/2.5/pe/ es_ES
dc.source Repositorio institucional - IGP es_ES
dc.subject Paleoclimatología--Perú es_ES
dc.subject Paleoclimatología--Holoceno es_ES
dc.subject Espeleotemas es_ES
dc.subject Climatología--Perú es_ES
dc.subject Precipitación (Meteorología)--Medición--Perú es_ES
dc.subject Geología estratigráfica--Perú es_ES
dc.subject Monzones--América del Sur es_ES
dc.subject Perú--Clima--Observaciones es_ES
dc.subject Perú--Geología--Observaciones es_ES
dc.subject Cuencas (Geología)--Perú es_ES
dc.title Hydroclimate variability of the South American Monsoon System during the last 1600 yr inferred from speleothem isotope records of the north-eastern Andes foothills in Peru es_ES
dc.type info:eu-repo/semantics/article es_ES
dc.subject.ocde Clima es_ES
dc.subject.ocde Hidrología es_ES
dc.subject.ocde Región andina es_ES
dc.subject.ocde Perú es_ES
dc.subject.ocde Geomorfología es_ES
dc.subject.ocde Océano Pacífico es_ES
dc.subject.ocde Precipitación es_ES
dc.subject.ocde Amazonía es_ES
dc.identifier.journal Climate of the Past (CP) - Discussions es_ES
dc.description.peer-review Por pares es_ES
dc.identifier.doi 10.5194/cpd-10-533-2014 es_ES

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