Results 121 to 130 of about 561 (169)

Sea-surface temperature extremes during the last interglacial

Cannings T, de Leau E, Stainbank S, Kocsis L, Kroon D, Spezzaferri S, Samankassou E.   +6 more
europepmc   +1 more source

Dynamic connectivities of plant metacommunities at a millennial time-scale: the Beringia testbed

Herzschuh U, Stoof-Leichsenring KR, Farkas LZ, Liu Y, Liu S, Böhmer T, Baisheva I, Biskaborn BK, Courtin J, Diekmann B, Epp LS, von Hippel B, Huang S, Huang Y, Jia W, Kaufman DS, Meyer H, Melles M, Meucci S, Pestryakova LA, Schulte L, Wagner B, Wang Z, Zakharov ES.   +23 more
europepmc   +1 more source

An evolutionary approach to human behaviour in the Palaeolithic: the diet breadth model and competition during MIS3 in France

, 2011
openaire   +1 more source

Ice Complex formation in arctic East Siberia during the MIS3 Interstadial [PDF]

Quaternary Science Reviews, 2014
Abstract A continuous 15 m long sequence of Ice Complex permafrost (Yedoma) exposed in a thermo-cirque at the southern coast of Bol'shoy Lyakhovsky Island (New Siberian Archipelago, Dmitry Laptev Strait) was studied to reconstruct past landscape and environmental dynamics. The sequence accumulated during the Marine Isotope Stage 3 (MIS3) Interstadial
Sebastian Wetterich, Lutz Schirrmeister, Vladimir Tumskoy   +2 more
exaly   +3 more sources

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On the sensitivity of the ocean response to LGM and MIS3-forcings

2023
The AMOC has undergone abrupt and quasi-periodic changes during the MIS-3. The prevailing background climatic conditions that produce such behavior in AMOC have yet to be fully understood. Previous studies have demonstrated that some climate models tend to have an oscillatory behavior in their AMOC under specific conditions that vary from model to ...
Chetankumar Jalihal, Ute Merkel, Matthias Prange, Uwe Mikolajewicz   +3 more
openaire   +1 more source

Characterising Dansgaard-Oeschger cycles: from MIS3 to today

2021
<p>One of the main contributors to palaeoclimate variability on millennial timescales is understood to be Dansgaard-Oeschger (D-O) cycles. Our awareness of these phenomena arises primarily from quasi-periodic, abrupt transitions of large magnitude detected in δ<sup>18</sup>O records from Greenland ...
Heather Andres, Lev Tarasov
openaire   +1 more source

Dansgaard-Oeschger events in climate models: A PMIP baseline MIS3 protocol

2022
<p>Frequent well documented Dansgaard-Oeschger (D-O) events occurred throughout the MIS3 period. This study lays the ground-work for a MIS3 D-O protocol for CMIP-class models. We consider the over-arching question: Are our models too stable?
Irene Malmierca Vallet, Louise C. Sime, Paul J. Valdes   +2 more
openaire   +1 more source

PROGLACIAL LAKE GAYHURST: MIS3 DEGLACIATION OF THE APPALACHIAN MOUNTAINS

Geological Society of America Abstracts with Programs, 2022
Olivier Caron, William W. Shilts, Michel Lamothe   +2 more
exaly   +2 more sources

Contrasting conditions preceding MIS3 and MIS2 Heinrich events

Global and Planetary Change, 2006
This paper presents an integrated multi-tracer study performed on piston cores recovered in the glacial ice-rafted detritus belt, stretching from Newfoundland to the Irish margin across the North Atlantic (40–55°N), in order to compare in detail the internal structure of each Heinrich event (HE). These tracers are IRD counts (quartz, dolomite, volcanic
Elsa Jullien, Francis E. Grousset, Sidney R. Hemming, Victoria L. Peck, Ian R. Hall, Cédric Jeantet, Isabelle Billy   +6 more
openaire   +1 more source

Forces driving ecological degradation in southern China during the MIS3: Natural or anthropogenic?

Palaeogeography, Palaeoclimatology, Palaeoecology
Qiong Chen, Zhongping Lai, Xiaoming Sun   +2 more
exaly   +2 more sources