Thermal impact of Heinrich stadials in cave temperature and speleothem oxygen isotope records

During each Heinrich stadial (HS), temperatures in southern Europe typically dropped several degrees during several hundred to few thousand years. We have developed a one-dimensional thermal conduction model that transfers the typical surface temperature anomaly of a HS to a series of hypothetical u...

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Veröffentlicht in:	Quaternary research 2021-05, Vol.101, p.37-50
Hauptverfasser:	Domínguez-Villar, David, Krklec, Kristina, López-Sáez, José Antonio, Sierro, Francisco J.
Format:	Artikel
Sprache:	eng
Schlagworte:	Cave art Caves Heat Heinrich Events Microclimate Oxygen isotopes Pleistocene Precipitation Proxies Sediments Surface temperature Thematic Set: Heinrich Events Tropical environments Ventilation
Online-Zugang:	Volltext
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