Please use this identifier to cite or link to this item: http://hdl.handle.net/2445/59424
Title: Hydrological evidence for a North Atlantic oscillation during the Little Ice Age outside its range observed since 1850.
Author: Martín Puertas, C.
Dorado Liñán, Isabel
Brauer, A.
Zorita, E.
Valero Garcés, Blas Lorenzo
Gutiérrez Merino, Emilia
Keywords: Dendrocronologia
Efecte del clima sobre les plantes
Pins
Climatologia
Dendrochronology
Vegetation and climate
Pine
Climatology
Issue Date: 2-Oct-2011
Publisher: European Geosciences Union (EGU)
Abstract: An annual-resolved precipitation reconstruction for the last 800 yr in Southern Spain has been performed using stable carbon isotope (δ13C) of Pinus nigra tree rings. The reconstruction exhibits high- to low-frequency variability and distinguishes a Little Ice Age (LIA, AD 1350<br>1850) characterized by lower averaged rainfall than both in the transition from the Medieval Climate Anomaly to the LIA and in the 20th century. The driest conditions are recorded during the Maunder solar Minimum (mid 17th<br>early 18th centuries), in good agreement with the Spanish documentary archive. Similar linkage between solar activity (maximum/minimum) and precipitation (increase/decrease) is observed throughout the entire LIA. Additionally, the relationship between the hydrological pattern in the Iberian Peninsula and Morocco during the LIA suggests different spatial distribution of precipitation in the south-eastern sector of the North Atlantic region such as it is known currently. Whereas in the instrumental record the precipitation evolves similarly in both regions and opposite to the North Atlantic oscillation (NAO) index, the coldest periods of the LIA shows a contrasting pattern with drier conditions in the South of Spain and wetter in Northern Africa. We suggest an extreme negative NAO conditions, accompanied by a southward excursion of the winter rainfall band beyond that observed in the last century, can explain this contrast. The sustained NAO conditions could have been triggered by solar minima and higher volcanic activity during the LIA.
Note: Reproducció del document publicat a: http://dx.doi.org/10.5194/cpd-7-4149-2011
It is part of: Climate of the Past Discussion, 2011, vol. 7, num. 6, p. 4149-4171
Related resource: http://dx.doi.org/10.5194/cpd-7-4149-2011
URI: http://hdl.handle.net/2445/59424
ISSN: 1814-9340
Appears in Collections:Articles publicats en revistes (Biologia Evolutiva, Ecologia i Ciències Ambientals)

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