FN Archimer Export Format
PT J
TI Early Holocene temperature variability in the Nordic Seas: The role of oceanic heat advection versus changes in orbital forcing
BT 
AF RISEBROBAKKEN, Bjorg
   DOKKEN, Trond
   SMEDSRUD, Lars Henrik
   ANDERSSON, Carin
   JANSEN, Eystein
   MOROS, Matthias
   IVANOVA, Elena V.
AS 1:1,5;2:1,5;3:1,5;4:1,4,5;5:1,4,5;6:1,3;7:2;
FF 1:;2:;3:;4:;5:;6:;7:;
C1 Univ Bergen, Bjerknes Ctr Climate Res, N-5007 Bergen, Norway.
   PP Shirshov Oceanol Inst, Moscow 117997, Russia.
   Inst Balt Sea Res, D-18119 Rostock, Germany.
   Univ Bergen, Dept Earth Sci, N-5007 Bergen, Norway.
   Uni Res, Uni Bjerknes Ctr, Bergen, Norway.
C2 UNIV BERGEN, NORWAY
   PP SHIRSHOV OCEANOL INST, RUSSIA
   INST BALT SEA RES, GERMANY
   UNIV BERGEN, NORWAY
   UNI RES BERGEN, NORWAY
IF 3.357
TC 80
UR https://archimer.ifremer.fr/doc/00227/33800/32547.pdf
   https://archimer.ifremer.fr/doc/00227/33800/32548.pdf
LA English
DT Article
CR IMAGES 1-MD101
   IMAGES V LEG 1-MD114
   IMAGES V LEG 4-MD114
BO Marion Dufresne
AB The separate roles of oceanic heat advection and orbital forcing on influencing early Holocene temperature variability in the eastern Nordic Seas is investigated. The effect of changing orbital forcing on the ocean temperatures is tested using the 1DICE model, and the 1DICE results are compared with new and previously published temperature reconstructions from a transect of five cores located underneath the pathway of Atlantic water, from the Faroe-Shetland Channel in the south to the Barents Sea in the north. The stronger early Holocene summer insolation at high northern latitudes increased the summer mixed layer temperatures, however, ocean temperatures underneath the summer mixed layer did not increase significantly. The absolute maximum in summer mixed layer temperatures occurred between 9 and 6 ka BP, representing the Holocene Thermal Maximum in the eastern Nordic Seas. In contrast, maximum in northward oceanic heat transport through the Norwegian Atlantic Current occurred approximately 10 ka BP. The maximum in oceanic heat transport at 10 ka BP occurred due to a major reorganization of the Atlantic Ocean circulation, entailing strong and deep rejuvenation of the Atlantic Meridional Overturning Circulation, combined with changes in the North Atlantic gyre dynamic causing enhanced transport of heat and salt into the Nordic Seas.
PY 2011
PD OCT
SO Paleoceanography
SN 0883-8305
PU Amer Geophysical Union
VL 26
IS 4 / PA4206
UT 000296160800001
BP 1
EP 17
DI 10.1029/2011PA002117
ID 33800
ER

EF