FN Archimer Export Format
PT J
TI Evidence for a three-phase sequence during Heinrich Stadial 4 using a multiproxy approach based on Greenland ice core records
BT 
AF GUILLEVIC, M.
   BAZIN, L.
   LANDAIS, A.
   STOWASSER, C.
   MASSON-DELMOTTE, V.
   BLUNIER, T.
   EYNAUD, F.
   FALOURD, S.
   MICHEL, E.
   MINSTER, B.
   POPP, T.
   PRIE, F.
   VINTHER, M.
AS 1:1,2;2:1;3:1;4:2;5:1;6:2;7:3;8:1;9:1;10:1;11:2;12:1;13:2;
FF 1:;2:;3:;4:;5:;6:;7:;8:;9:;10:;11:;12:;13:;
C1 UMR CEA CNRS UVSQ 8212, Lab Sci Climat & Environm, Gif Sur Yvette, France.
   Univ Copenhagen, Niels Bohr Inst, Ctr Ice & Climate, DK-2100 Copenhagen, Denmark.
   Univ Bordeaux 1, UMR CNRS EPOC OASU 5805, Lab EPOC, F-33405 Talence, France.
C2 CEA, FRANCE
   UNIV COPENHAGEN, DENMARK
   UNIV BORDEAUX, FRANCE
IN DOAJ
IF 3.382
TC 40
UR https://archimer.ifremer.fr/doc/00293/40438/39539.pdf
   https://archimer.ifremer.fr/doc/00293/40438/39540.zip
   https://archimer.ifremer.fr/doc/00293/40438/71310.pdf
LA English
DT Article
CR IMAGES 1-MD101
   MD 142 / ALIENOR 2
BO Marion Dufresne
AB Glacial climate was characterised by two types of abrupt events. Greenland ice cores record Dansgaard–Oeschger events, marked by abrupt warming in-between cold, stadial phases. Six of these stadials appear related to major Heinrich events (HEs), identified from ice-rafted debris (IRD) and large excursions in carbon- and oxygen-stable isotopic ratios in North Atlantic deep sea sediments, documenting major ice sheet collapse events. This finding has led to the paradigm that glacial cold events are induced by the response of the Atlantic Meridional Overturning Circulation to such massive freshwater inputs, supported by sensitivity studies conducted with climate models of various complexities. These models also simulate synchronous Greenland temperature and lower-latitude hydrological changes.
PY 2014
PD DEC
SO Climate Of The Past
SN 1814-9324
PU Copernicus Gesellschaft Mbh
VL 10
IS 6
UT 000347569500010
BP 2115
EP 2133
DI 10.5194/cp-10-2115-2014
ID 40438
ER

EF