FN Archimer Export Format
PT J
TI Full-depth temperature trends in the northeastern Atlantic through the early 21st century
BT 
AF DESBRUYERES, Damien
   MCDONAGH, E. L.
   KING, B. A.
   GARRY, F. K.
   BLAKER, A. T.
   MOAT, B. I.
   MERCIER, Herle
AS 1:1;2:1;3:1;4:2;5:1;6:1;7:3;
FF 1:;2:;3:;4:;5:;6:;7:;
C1 Natl Oceanog Ctr, Southampton, Hants, England.
   Univ Southampton, Natl Oceanog Ctr, Sch Ocean & Earth Sci, Southampton, Hants, England.
   CNRS Ifremer UBO IRD, UMR 6523, Lab Phys Oceans, Plouzane, France.
C2 NOC, UK
   NOC, UK
   CNRS, FRANCE
IF 4.196
TC 23
UR https://archimer.ifremer.fr/doc/00236/34677/33026.pdf
LA English
DT Article
CR OVIDE 1
   OVIDE 2
   OVIDE 3
   OVIDE 4
   OVIDE 5
BO Thalassa
   Maria S. Merian
DE ;North Atlantic;temperature;observations;hiatus
AB The vertical structure of temperature trends in the northeastern Atlantic (NEA) is investigated using a blend of Argo and hydrography data. The representativeness of sparse hydrography sampling in the basin mean is assessed using a numerical model. Between 2003 and 2013, the NEA underwent a strong surface cooling (0–450 m) and a significant warming at intermediate and deep levels (1000 m to 3000 m) that followed a strong cooling trend observed between 1988 and 2003. During 2003–2013, gyre-specific changes are found in the upper 1000 m (warming and cooling of the subtropical and subpolar gyres, respectively), while the intermediate and deep warming primarily occurred in the subpolar gyre, with important contributions from isopycnal heave and water mass property changes. The full-depth temperature change requires a local downward heat flux of 0.53 ± 0.06 W m−2 through the sea surface, and its vertical distribution highlights the likely important role of the NEA in the recent global warming hiatus.
PY 2014
PD NOV
SO Geophysical Research Letters
SN 0094-8276
PU Amer Geophysical Union
VL 41
IS 22
UT 000346644600028
BP 7971
EP 7979
DI 10.1002/2014GL061844
ID 34677
ER

EF