3800 years of quantitative precipitation reconstruction from the northwest Yucatan Peninsula
Por: Carrillo Bastos, Alicia [autor/a]
.
Islebe, Gerald A [autor/a]
| Torrescano Valle, Nuria [autor/a]
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Tipo de material: ![Artículo
en línea](/opac-tmpl/lib/famfamfam/AR.png)
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Tipo de ítem | Biblioteca actual | Colección | Signatura | Estado | Fecha de vencimiento | Código de barras |
---|---|---|---|---|---|---|
Artículos | Biblioteca Electrónica Recursos en línea (RE) | ECOSUR | Recurso digital | ECO400531134570 |
Acceso en línea sin restricciones
Precipitation over the last 3800 years has been reconstructed using modern pollen calibration and precipitation data. A transfer function was then performed via the linear method of partial least squares. By calculating precipitation anomalies, it is estimated that precipitation deficits were greater than surpluses, reaching 21% and ,9%, respectively. The period from 50 BC to 800 AD was the driest of the record. The drought related to the abandonment of the Maya Preclassic period featured a 21% reduction in precipitation, while the drought of the Maya collapse (800 to 860 AD) featured a reduction of 18%. The Medieval Climatic Anomaly was a period of positive phases (3.8-7.6%). The Little Ice Age was a period of climatic variability, with reductions in precipitation but without deficits. eng
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