Full-depth temperature trends in the northeastern Atlantic through the early 21st century

International audience 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 N...

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Bibliographic Details
Published in:Geophysical Research Letters
Main Authors: Desbruyères, D. G., Mcdonagh, E. L., King, B. A., Garry, F. K., Blaker, A. T., Moat, B. I., Mercier, H.
Other Authors: National Oceanography Centre Southampton (NOC), University of Southampton, Ocean and Earth Science Southampton, University of Southampton-National Oceanography Centre (NOC), Laboratoire de physique des océans (LPO), Institut de Recherche pour le Développement (IRD)-Institut Français de Recherche pour l'Exploitation de la Mer (IFREMER)-Université de Brest (UBO)-Centre National de la Recherche Scientifique (CNRS)
Format: Article in Journal/Newspaper
Language:English
Published: HAL CCSD 2014
Subjects:
North Atlantic
temperature
observations
hiatus
[SDU.STU.OC]Sciences of the Universe [physics]/Earth Sciences/Oceanography
[SDU.OCEAN]Sciences of the Universe [physics]/Ocean
Atmosphere
Online Access:https://hal.science/hal-01129001
https://doi.org/10.1002/2014GL061844
Description
Summary:International audience 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.

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