FN Archimer Export Format
PT J
TI Multicentennial Agulhas leakage variability and links to North Atlantic climate during the past 80,000 years
BT 
AF DYEZ, Kelsey A.
   ZAHN, Rainer
   HALL, Ian R.
AS 1:1;2:1,2;3:3;
FF 1:;2:;3:;
C1 Univ Autonoma Barcelona, Inst Ciencia & Tecnol Ambientals, Bellaterra, Spain.
   Univ Autonoma Barcelona, Inst Catalana Recerca & Estudis Avancats, Dept Fis, Bellaterra, Spain.
   Cardiff Univ, Sch Earth & Ocean Sci, Cardiff CF10 3AX, S Glam, Wales.
C2 UNIV AUTONOMA BARCELONA, SPAIN
   UNIV AUTONOMA BARCELONA, SPAIN
   UNIV CARDIFF, UK
IF 3.738
TC 26
UR https://archimer.ifremer.fr/doc/00289/40041/39390.pdf
   https://archimer.ifremer.fr/doc/00289/40041/39391.docx
   https://archimer.ifremer.fr/doc/00289/40041/39392.pdf
   https://archimer.ifremer.fr/doc/00289/40041/39393.pdf
   https://archimer.ifremer.fr/doc/00289/40041/39394.pdf
   https://archimer.ifremer.fr/doc/00289/40041/39396.pdf
   https://archimer.ifremer.fr/doc/00289/40041/39397.pdf
   https://archimer.ifremer.fr/doc/00289/40041/39398.pdf
LA English
DT Article
CR IMAGES 3-IPHIS-MD106
   MD 123 / GEOSCIENCES 1
   MD 128 / SWAF
   NAUSICAA-IMAGES 2-MD105
BO Marion Dufresne
DE ;Agulhas leakage;SST
AB New high-resolution sea surface temperature (SST) and sea surface salinity (SSS) estimates are presented from the Agulhas Bank slope in the Atlantic sector of the Agulhas Corridor using planktic foraminiferal (Globigerinoides ruber) O-18 and Mg/Ca-derived SST. By focusing on the last 80,000years, this is the first fine-scale Agulhas leakage record that overlaps in time with much of the Greenland ice core record of abrupt climate changes in the North Atlantic region. The multicentennial profiles indicate instances of warm SST and/or increased SSS coincident with Northern Hemisphere cool periods, followed by Northern Hemisphere warming. These periods of enhanced SST and SSS in the Agulhas Corridor occur at the last glacial termination (T1) and during North Atlantic cold episodes associated with Heinrich (H) meltwater events. To a first-order approximation, the timing of maximal salinity events in relation to periods of North Atlantic freshwater perturbation is consistent with the concept suggested by climate models that enhanced Agulhas leakage provides for buoyancy compensation and can potentially trigger increased convective activity in the North Atlantic, thereby restoring Atlantic overturning circulation after relatively weak states.
PY 2014
PD DEC
SO Paleoceanography
SN 0883-8305
PU Amer Geophysical Union
VL 29
IS 12
UT 000348536600008
BP 1238
EP 1248
DI 10.1002/2014PA002698
ID 40041
ER

EF