FN Archimer Export Format
PT J
TI Inception of the Northern European ice sheet due to contrasting ocean and insolation forcing
BT 
AF RISEBROBAKKEN, Bjorg
   DOKKEN, Trond
   OTTERA, Odd Helge
   JANSEN, Eystein
   GAO, Yongqi
   DRANGE, Helge
AS 1:1,2;2:1;3:1,3;4:1,2;5:1,3;6:1,3;
FF 1:;2:;3:;4:;5:;6:;
C1 Bjerkness Ctr Climate Res, N-5007 Bergen, Norway.
   Univ Bergen, Dept Earth Sci, N-5007 Bergen, Norway.
   Nansen Environm & Remote Sensing Ctr, N-5006 Bergen, Norway.
C2 BCCR, NORWAY
   UNIV BERGEN, NORWAY
   NERSC, NORWAY
IF 2.224
TC 31
UR https://archimer.ifremer.fr/doc/00233/34441/82768.pdf
LA English
DT Article
CR IMAGES 1-MD101
   IMAGES V LEG 1-MD114
   IMAGES V LEG 4-MD114
BO Marion Dufresne
DE ;glacial inception;Nordic Seas;Northern European ice sheets;palco-reconstruction;OGCM;AMOC;insolation;insolation gradient
AB About 115,000 yr ago the last interglacial reached its terminus and nucleation of new ice-sheet growth was initiated. Evidence from the northernmost Nordic Seas indicate that the inception of the last glacial was related to an intensification of the Atlantic Meridional Overturning Circulation (AMOC) in its northern limb. The enhanced AMOC, combined with minimum Northern hemisphere insolation, introduced a strong sea-land thermal gradient that, together with a strong wintertime latitudinal insolation gradient, increased the storminess and moisture transport to the high Northern European latitudes at a time when the Northern hemisphere summer insolation approached its minimum.
PY 2007
PD JAN
SO Quaternary Research
SN 0033-5894
PU Academic Press Inc Elsevier Science
VL 67
IS 1
UT 000243893800011
BP 128
EP 135
DI 10.1016/j.yqres.2006.07.007
ID 34441
ER

EF