Articles | Volume 16, issue 1
https://doi.org/10.5194/cp-16-29-2020
© Author(s) 2020. This work is distributed under
the Creative Commons Attribution 4.0 License.
the Creative Commons Attribution 4.0 License.
https://doi.org/10.5194/cp-16-29-2020
© Author(s) 2020. This work is distributed under
the Creative Commons Attribution 4.0 License.
the Creative Commons Attribution 4.0 License.
NALPS19: sub-orbital-scale climate variability recorded in northern Alpine speleothems during the last glacial period
Institute of Geology, University of Innsbruck, Innrain 52, 6020
Innsbruck, Austria
Christoph Spötl
Institute of Geology, University of Innsbruck, Innrain 52, 6020
Innsbruck, Austria
Susanne Brandstätter
Institute of Geology, University of Innsbruck, Innrain 52, 6020
Innsbruck, Austria
Tobias Erhardt
Climate and Environmental Physics and Oeschger Center for Climate
Change Research, University of Bern, Sidlerstrasse 5, 3012 Bern, Switzerland
Marc Luetscher
Institute of Geology, University of Innsbruck, Innrain 52, 6020
Innsbruck, Austria
Swiss Institute for Speleology and Karst Studies (SISKA), 2301 La
Chaux-de-Fonds, Switzerland
R. Lawrence Edwards
School of Earth Sciences, University of Minnesota, John T. Tate Hall, 116 Church Street SE, Minneapolis, MN 55455-0149, USA
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Latest update: 17 Nov 2024
Short summary
Abrupt climate change during the last ice age can be used to provide important insights into the timescales on which the climate is capable of changing and the mechanisms that drive those changes. In this study, we construct climate records for the period 60 to 120 ka using stalagmites that formed in caves along the northern rim of the European Alps and find good agreement with the timing of climate changes in Greenland and the Asian monsoon.
Abrupt climate change during the last ice age can be used to provide important insights into the...