FN Archimer Export Format
PT C
TI A complex North Atlantic permanent pycnocline revealed by Argo data
BT 
AF FEUCHER, Charlene
   MAZE, Guillaume
   MERCIER, Herle
AS 1:1;2:1;3:1;
FF 1:PDG-ODE-LPO;2:PDG-ODE-LPO;3:;
C1 Ifremer, Laboratoire de Physique des Océans, France
C2 IFREMER, FRANCE
SI BREST
SE PDG-ODE-LPO
UR https://archimer.ifremer.fr/doc/00257/36818/35450.pdf
LA English
DT Poster
AB In the North Atlantic subtropical gyre, the oceanic vertical structure of density is characterized by a region of rapid increase with depth. This layer is called the permanent pycnocline. The pycnocline is the transition layer between light, low-latitude, surface water masses which are ventilated every winter when penetrated locally by the mixed layer and dense, deeper water masses whose properties are set in the high latitudes.  Assessing the structure and variability of the permanent pycnocline is of a major interest in the under- standing of the climate system because the pycnocline embeds the warm water sphere and most of the wind-forced horizontal circulation.  We characterized the large scale structure of the permanent pycnocline with in-situ data from the Argo ar- ray. We developed a new method to objectively characterize its properties (depth, thickness, temperature, salinity, density, potential vorticity). Results reveal a surprisingly complex structure with inhomogeneous properties. In the Gulf Stream recirculation region the pycnocline is deep, thick, the maximum of stratification is found in the middle on the layer and follow an isopycnal surface. But away from this textbook regional description, the pycnocline is characterized by vertical asymmetries and gradients in thermohaline properties. T/S distribution along the permanent pycnocline depth reveals a diversity of water masses.  We will present the mean observed structure and properties of the permanent pycnocline and relate them to physical processes that constraint them.
PY 2015
PD APR
ID 36818
ER

EF