FN Archimer Export Format
PT J
TI Locally and Remotely Forced Subtropical AMOC Variability: A Matter of Time Scales
BT 
AF JAMET, Quentin
   DEWAR, William K.
   WIENDERS, Nicolas
   DEREMBLE, Bruno
   CLOSE, Sally
   PENDUFF, Thierry
AS 1:1;2:1,2;3:2;4:3;5:4;6:1;
FF 1:;2:;3:;4:;5:;6:;
C1 Univ Grenoble Alpes, CNRS, IRD, Grenoble INP,IGE, Grenoble, France.
   Florida State Univ, Dept Earth Ocean & Atmospher Sci, Tallahassee, FL 32306 USA.
   Lab Meteorol Dynam, Paris, France.
   Univ Bretagne Occident, Lab Oceanog Phys & Spatiale, Brest, France.
C2 UNIV GRENOBLE ALPES, FRANCE
   UNIV FLORIDA STATE, USA
   LAB METEOROL DYNAM, FRANCE
   UBO, FRANCE
UM LOPS
IN WOS Cotutelle UMR
   copubli-france
   copubli-univ-france
   copubli-int-hors-europe
IF 5.148
TC 9
UR https://archimer.ifremer.fr/doc/00695/80736/84545.pdf
LA English
DT Article
DE ;North Atlantic Ocean;Meridional overturning circulation;Ensembles;Ocean models;Climate variability
AB Mechanisms driving the North Atlantic meridional overturning circulation (AMOC) variability at low frequency are of central interest for accurate climate predictions. Although the subpolar gyre region has been identified as a preferred place for generating climate time-scale signals, their southward propagation remains under consideration, complicating the interpretation of the observed time series provided by the Rapid Climate Change-Meridional Overturning Circulation and Heatflux Array-Western Boundary Time Series (RAPID-MOCHA-WBTS) program. In this study, we aim at disentangling the respective contribution of the local atmospheric forcing from signals of remote origin for the subtropical low-frequency AMOC variability. We analyze for this a set of four ensembles of a regional (20 degrees S-55 degrees N), eddy-resolving (1/12 degrees) North Atlantic oceanic configuration, where surface forcing and open boundary conditions are alternatively permuted from fully varying (realistic) to yearly repeating signals. Their analysis reveals the predominance of local, atmospherically forced signal at interannual time scales (2-10 years), whereas signals imposed by the boundaries are responsible for the decadal (10-30 years) part of the spectrum. Due to this marked time-scale separation, we show that, although the intergyre region exhibits peculiarities, most of the subtropical AMOC variability can be understood as a linear superposition of these two signals. Finally, we find that the decadal-scale, boundary-forced AMOC variability has both northern and southern origins, although the former dominates over the latter, including at the site of the RAPID array (26.5 degrees N).
PY 2020
PD JUL
SO Journal Of Climate
SN 0894-8755
PU Amer Meteorological Soc
VL 33
IS 12
UT 000537891600011
BP 5155
EP 5172
DI 10.1175/JCLI-D-19-0844.1
ID 80736
ER

EF