Por favor, use este identificador para citar o enlazar a este item: http://hdl.handle.net/10261/47766
COMPARTIR / EXPORTAR:
logo share SHARE logo core CORE BASE
Visualizar otros formatos: MARC | Dublin Core | RDF | ORE | MODS | METS | DIDL | DATACITE

Invitar a revisión por pares abierta
Título

A multi-proxy perspective on millennium-long climate variability in the Southern Pyrenees

AutorMorellón, Mario CSIC ORCID; Pérez-Sanz, Ana CSIC; Corella, Juan Pablo CSIC ORCID; González-Sampériz, Penélope CSIC ORCID ; Moreno Caballud, Ana CSIC ORCID ; López Sáez, José Antonio CSIC ORCID ; Valero-Garcés, Blas L. CSIC ORCID
Fecha de publicación30-mar-2012
EditorEuropean Geosciences Union
CitaciónClimate of the Past 8: 683–700 (2012)
ResumenThis paper reviews multi-proxy paleoclimatic reconstructions with robust age-control derived from lacustrine, dendrochronological and geomorphological records and characterizes the main environmental changes that occurred in the Southern Pyrenees during the last millennium. Warmer and relatively arid conditions prevailed during the Medieval Climate Anomaly (MCA, ca. 900–1300 AD), with a significant development of xerophytes and Mediterranean vegetation and limited deciduous tree formations (mesophytes). The Little Ice Age (LIA, 1300–1800 AD) was generally colder and moister, with an expansion of deciduous taxa and cold-adapted montane conifers. Two major phases occurred within this period: (i) a transition MCA–LIA, characterized by fluctuating, moist conditions and relatively cold temperatures (ca. 1300 and 1600 AD); and (ii) a second period, characterized by the coldest and most humid conditions, coinciding with maximum (recent) glacier advances (ca. 1600–1800 AD). Glaciers retreated after the LIA when warmer and more arid conditions dominated, interrupted by a short-living cooling episode during the late 19th to early 20th centuries. Some records suggest a response to solar activity with colder and slightly moister conditions during solar minima. Centennial-scale hydrological fluctuations are in phase with reconstructions of NAO variability, which appears to be one of the main climate mechanisms influencing rainfall variations in the region during the last millennium.
Descripción18 páginas, 1 tabla, 3 figuras
Versión del editorhttp://dx.doi.org/10.5194/cp-8-683-2012
URIhttp://hdl.handle.net/10261/47766
DOI10.5194/cp-8-683-2012
ISSN1814-9324
E-ISSN1814-9332
Aparece en las colecciones: (IPE) Artículos
(CEAB) Artículos
(CCHS-IH) Artículos




Ficheros en este ítem:
Mostrar el registro completo

CORE Recommender

SCOPUSTM   
Citations

78
checked on 25-mar-2024

WEB OF SCIENCETM
Citations

70
checked on 23-feb-2024

Page view(s)

561
checked on 28-mar-2024

Download(s)

309
checked on 28-mar-2024

Google ScholarTM

Check

Altmetric

Altmetric


NOTA: Los ítems de Digital.CSIC están protegidos por copyright, con todos los derechos reservados, a menos que se indique lo contrario.