FN Archimer Export Format
PT J
TI Absence of an internal multidecadal oscillation in the North Atlantic has consequences for anticipating the future of marine ecosystems
BT 
AF Beaugrand, G
   Faillettaz, Robin
   Kirby, R.R.
AS 1:1;2:2;3:3,4;
FF 1:;2:PDG-RBE-STH-LTBH;3:;
C1 Centre National de la Recherche Scientifique, Laboratoire d’Océanologie et de Géosciences, Station marine de Wimereux, Université de Lille, 28 avenue Foch, 62930 Wimereux, France
   Ifremer, STH, Laboratoire de Technologie et de Biologie Halieutique, 8 rue François Toullec, 56100 Lorient, France
   The Secchi Disk Foundation, Kiln Cottage, Gnaton, Yealmpton, Devon PL8 2HU, UK
   Ronin Institute, Montclair, NJ 07043, USA
C2 CNRS, FRANCE
   IFREMER, FRANCE
   THE SECCHI DISK FND, UK
   RONIN INST, USA
SI LORIENT
SE PDG-RBE-STH-LTBH
IN WOS Ifremer UPR
   copubli-france
   copubli-europe
   copubli-int-hors-europe
IF 1.459
TC 1
UR https://archimer.ifremer.fr/doc/00742/85414/109254.pdf
LA English
DT Article
DE ;Climate change;Russell Cycle;Bluefin tuna;Sea surface temperature;AMO
AB The North Atlantic marine ecosystem has been expected to adjust imminently to a negative phase of the Atlantic Multidecadal Oscillation (AMO). Recent results suggest, however, that the AMO is not a regular internal source of variability, but has been driven by both volcanism and sulphate aerosol emissions that have influenced temperature negatively, and a period of greenhouse gas accumulation causing temperatures to be higher than normal. The demise of the AMO removes the expected and imminent cyclical change from the current warm phase to a negative cool phase in the North Atlantic. Here, we discuss the implications of this new finding for the near-future of North Atlantic marine ecosystems in a context of rapid climate warming. 
PY 2021
SO Climate Research
SN 0936-577X
PU Inter-Research Science Center
VL 85
UT 000751732200007
BP 107
EP 111
DI 10.3354/cr01676
ID 85414
ER

EF