FN Archimer Export Format
PT J
TI Recent changes in the Greenland-Scotland overflow-derived water transport inferred from hydrographic observations in the southern Irminger Sea
BT 
AF SARAFANOV, Artem
   FALINA, Anastasia
   MERCIER, Herle
   LHERMINIER, Pascale
   SOKOV, Alexey
AS 1:1;2:1;3:2;4:2;5:1;
FF 1:;2:;3:;4:PDG-DOP-DCB-OPS-LPO;5:;
C1 PP Shirshov Oceanol Inst, Moscow 117997, Russia.
   CNRS, UBO, IRD,Lab Phys Oceans, IFREMER,UMR 6523, F-29280 Plouzane, France.
C2 PP SHIRSHOV OCEANOL INST, RUSSIA
   CNRS, FRANCE
   IFREMER, FRANCE
SI BREST
SE PDG-DPCP
   PDG-DOP-DCB-OPS-LPO
IN WOS Ifremer jusqu'en 2018
   copubli-france
   copubli-int-hors-europe
IF 3.204
TC 21
TU Centre national de la recherche scientifique
   Institut de recherche pour le développement
   Institut français de recherche pour l'exploitation de la mer
   Université de Bretagne Occidentale
UR https://archimer.ifremer.fr/doc/2009/publication-6633.pdf
LA English
DT Article
CR OVIDE 1
   OVIDE 2
   OVIDE 3
BO Thalassa
   Maria S. Merian
AB Recent decadal changes (1955-2007) in the baroclinic transport (TBC) of the Deep Western Boundary Current (DWBC) carrying the Greenland-Scotland overflow-derived waters along the East Greenland slope are quantified from a set of hydrographic sections in vicinity of Cape Farewell. The updated historical record of TBC shows clear decadal variability (+/- 2-2.5 Sv) with the transport minima in the 1950s and mid-1990s, maximum in the early 1980s and moderate-to-high transport in the 2000s. Since the mid-1990s, the DWBC TBC has increased by similar to 2 Sv (significant at the 99.9% level), which constitute similar to 20% of the mean absolute transport (9.0 Sv) as obtained from three cruises in 2002-2006. The DWBC TBC anomalies negatively correlate (R = -0.80) with thickness anomalies of the Labrador Sea Water (LSW) at its origin implying a close association, albeit not necessarily causative, between the DWBC transport east of Greenland and the LSW production.
PY 2009
PD JUN
SO Geophysical Research Letters ( GRL )
SN 0094-8276
PU American Geophysical Union
VL 36
IS L13606
UT 000267935200001
BP 1
EP 6
DI 10.1029/2009GL038385
ID 6633
ER

EF