FN Archimer Export Format
PT J
TI Fast and slow components of interstadial warming in the North Atlantic during the last glacial
BT 
AF Margari, Vasiliki
   Skinner, Luke C.
   Menviel, Laurie
   Capron, Emilie
   Rhodes, Rachael H.
   Mleneck-Vautravers, Maryline J.
   Ezat, Mohamed M.
   Martrat, Belen
   Grimalt, Joan O.
   Hodell, David A.
   Tzedakis, Polychronis C.
AS 1:1;2:2;3:3;4:4;5:2;6:2;7:2,5,6;8:7;9:7;10:2;11:1;
FF 1:;2:;3:;4:;5:;6:;7:;8:;9:;10:;11:;
C1 Environmental Change Research Centre, Department of Geography, University College London, London, WC1E 6BT, UK
   Department of Earth Sciences, University of Cambridge, Cambridge, CB2 3EQ, UK
   Climate Change Research Centre, PANGEA, The University of New South Wales, Sydney, NSW, 2052, Australia
   Physics of Ice, Climate, Earth, Niels Bohr Institute, University of Copenhagen, Tagensvej 16, DK-2200, Copenhagen, Denmark
   CAGE-Centre for Arctic Gas Hydrate, Environment and Climate, Department of Geosciences, UiT The Arctic University of Norway, 9037, Tromsø, Norway
   Department of Geology, Faculty of Science, Beni-Suef University, Beni-Suef, Egypt
   Department of Environmental Chemistry, Institute of Environmental Assessment and Water Research (IDAEA), Spanish Council for Scientific Research (CSIC), 08034, Barcelona, Spain
C2 UNIV COLL LONDON, UK
   UNIV CAMBRIDGE, UK
   UNIV NEW S WALES, AUSTRALIA
   UNIV COPENHAGEN, DENMARK
   UNIV ARCTIC UIT NORWAY, NORWAY
   UNIV BENI-SUEF, EGYPT
   CSIC, SPAIN
IN DOAJ
IF 7.29
TC 7
UR https://archimer.ifremer.fr/doc/00643/75476/76313.pdf
   https://archimer.ifremer.fr/doc/00643/75476/76314.pdf
   https://archimer.ifremer.fr/doc/00643/75476/76315.pdf
   https://archimer.ifremer.fr/doc/00643/75476/76316.xlsx
   https://archimer.ifremer.fr/doc/00643/75476/76317.pdf
LA English
DT Article
CR MD 123 / GEOSCIENCES 1
BO Marion Dufresne
AB The abrupt nature of warming events recorded in Greenland ice-cores during the last glacial has generated much debate over their underlying mechanisms. Here, we present joint marine and terrestrial analyses from the Portuguese Margin, showing a succession of cold stadials and warm interstadials over the interval 35–57 ka. Heinrich stadials 4 and 5 contain considerable structure, with a short transitional phase leading to an interval of maximum cooling and aridity, followed by slowly increasing sea-surface temperatures and moisture availability. A climate model experiment reproduces the changes in western Iberia during the final part of Heinrich stadial 4 as a result of the gradual recovery of the Atlantic meridional overturning circulation. What emerges is that Greenland ice-core records do not provide a unique template for warming events, which involved the operation of both fast and slow components of the coupled atmosphere–ocean–sea-ice system, producing adjustments over a range of timescales. 
PY 2020
PD AUG
SO Communications Earth & Environment
SN 2662-4435
PU Springer Science and Business Media LLC
VL 1
IS 1
UT 000648605100006
DI 10.1038/s43247-020-0006-x
ID 75476
ER

EF