FN Archimer Export Format
PT J
TI A signal of persistent Atlantic multidecadal variability in Arctic sea ice
BT 
AF MILES, Martin W.
   DIVINE, Dmitry V.
   FUREVIK, Tore
   JANSEN, Eystein
   MOROS, Matthias
   OGILVIE, Astrid E. J.
AS 1:1,2,3;2:4,5;3:2,6;4:1,2,7;5:8;6:3;
FF 1:;2:;3:;4:;5:;6:;
C1 Uni Res, Bergen, Norway.
   Bjerknes Ctr Climate Res, Bergen, Norway.
   Univ Colorado, Inst Arctic & Alpine Res, Boulder, CO 80309 USA.
   Norwegian Polar Res Inst, Polar Environm Ctr, Tromso, Norway.
   Univ Tromso, Dept Math & Stat, Tromso, Norway.
   Univ Bergen, Inst Geophys, Bergen, Norway.
   Univ Bergen, Dept Earth Sci, Bergen, Norway.
   Balt Sea Res Inst, Rostock, Germany.
C2 UNI RES BERGEN, NORWAY
   BCCR, NORWAY
   UNIV COLORADO BOULDER, USA
   NORWEGIAN POLAR INST, NORWAY
   UNIV TROMSO, NORWAY
   UNIV BERGEN, NORWAY
   UNIV BERGEN, NORWAY
   LEIBNIZ INST BALT SEA RES (IOW), GERMANY
IF 4.196
TC 98
UR https://archimer.ifremer.fr/doc/00291/40199/39229.pdf
   https://archimer.ifremer.fr/doc/00291/40199/39230.txt
   https://archimer.ifremer.fr/doc/00291/40199/39232.pdf
LA English
DT Article
CR IMAGES V LEG 1-MD114
   IMAGES V LEG 4-MD114
BO Marion Dufresne
DE ;sea ice
AB Satellite data suggest an Arctic sea ice-climate system in rapid transformation, yet its long-term natural modes of variability are poorly known. Here we integrate and synthesize a set of multicentury historical records of Atlantic Arctic sea ice, supplemented with high-resolution paleoproxy records, each reflecting primarily winter/spring sea ice conditions. We establish a signal of pervasive and persistent multidecadal (~60–90 year) fluctuations that is most pronounced in the Greenland Sea and weakens further away. Covariability between sea ice and Atlantic multidecadal variability as represented by the Atlantic Multidecadal Oscillation (AMO) index is evident during the instrumental record, including an abrupt change at the onset of the early twentieth century warming. Similar covariability through previous centuries is evident from comparison of the longest historical sea ice records and paleoproxy reconstructions of sea ice and the AMO. This observational evidence supports recent modeling studies that have suggested that Arctic sea ice is intrinsically linked to Atlantic multidecadal variability. This may have implications for understanding the recent negative trend in Arctic winter sea ice extent, although because the losses have been greater in summer, other processes and feedbacks are also important.
PY 2014
PD JAN
SO Geophysical Research Letters
SN 0094-8276
PU Amer Geophysical Union
VL 41
IS 2
UT 000332991000038
BP 463
EP 469
DI 10.1002/2013GL058084
ID 40199
ER

EF