FN Archimer Export Format
PT J
TI Regional seesaw between the North Atlantic and Nordic Seas during the last glacial abrupt climate events
BT 
AF WARY, Melanie
   EYNAUD, Frederique
   SWINGEDOUW, Didier
   MASSON-DELMOTTE, Valerie
   MATTHIESSEN, Jens
   KISSEL, Catherine
   ZUMAQUE, Jena
   ROSSIGNOL, Linda
   JOUZEL, Jean
AS 1:1;2:1;3:1;4:2;5:3;6:2;7:1,4;8:1;9:2;
FF 1:;2:;3:;4:;5:;6:;7:;8:;9:;
C1 Univ Bordeaux, EPHE, CNRS, UMR 5805,EPOC, F-33615 Pessac, France.
   UVSQ, INSU, CNRS, UMR8212,LSCE,IPSL,CEA, F-91191 Gif Sur Yvette, France.
   Helmholtz Ctr Polar & Marine Res, Alfred Wegener Inst, D-27568 Bremerhaven, Germany.
   Univ Quebec Montreal, Geotop, Montreal, PQ H3C 3P8, Canada.
C2 UNIV BORDEAUX, FRANCE
   UNIV VERSAILLES, FRANCE
   INST A WEGENER, GERMANY
   UNIV QUEBEC, CANADA
IN DOAJ
IF 3.174
TC 10
UR https://archimer.ifremer.fr/doc/00420/53149/55328.pdf
   https://archimer.ifremer.fr/doc/00420/53149/55329.pdf
LA English
DT Article
CR IMAGES 1-MD101
   IMAGES V LEG 1-MD114
   IMAGES V LEG 4-MD114
BO Marion Dufresne
AB Dansgaard-Oeschger oscillations constitute one of the most enigmatic features of the last glacial cycle. Their cold atmospheric phases have been commonly associated with cold sea-surface temperatures and expansion of sea ice in the North Atlantic and adjacent seas. Here, based on dinocyst analyses from the 48-30 ka interval of four sediment cores from the northern Northeast Atlantic and southern Norwegian Sea, we provide direct and quantitative evidence of a regional paradoxical seesaw pattern: cold Greenland and North Atlantic phases coincide with warmer sea-surface conditions and shorter seasonal sea-ice cover durations in the Norwegian Sea as compared to warm phases. Combined with additional palaeorecords and multi-model hosing simulations, our results suggest that during cold Greenland phases, reduced Atlantic meridional overturning circulation and cold North Atlantic sea-surface conditions were accompanied by the subsurface propagation of warm Atlantic waters that re-emerged in the Nordic Seas and provided moisture towards Greenland summit. 
PY 2017
PD JUL
SO Climate Of The Past
SN 1814-9324
PU Copernicus Gesellschaft Mbh
VL 13
IS 6
UT 000404777800001
BP 729
EP 739
DI 10.5194/cp-13-729-2017
ID 53149
ER

EF