FN Archimer Export Format
PT J
TI Spatial and Seasonal Variability of Mixed Layer Depth in the Tropical Atlantic at 10 °W using 40 Years of Observation Data
BT 
AF Kouame Kanga, Désiré
   Kouassi Aka, Marcel
   Trokourey, Albert
   Toualy, Elisée
   N’guessan, Benjamin K.
   BREHMER, Patrice
   Ostrowski, Marek
AS 1:1;2:1;3:2;4:3;5:1,2;6:4;7:5;
FF 1:;2:;3:;4:;5:;6:;7:;
C1 Centre de Recherches Océanologiques (CRO), 29 Rue des Pêcheurs Treichville BPV 18 Abidjan, Côte d’Ivoire
   Université Felix Houphouët-Boigny, Laboratoire de Chimie Physique UFR SSMT, 22 BP 582 Abidjan 22, Côte d’Ivoire
   Laboratoire de Physique de l'Atmosphère et de Mécanique des Fluides (LAPA-MF) UFR SSMT, 22 BP 582 Abidjan 22, Côte d’Ivoire
   IRD, Univ Brest, CNRS, Ifremer, Lemar Délégation Régionale IRD Ouest Plouzané, France
   Institute of Marine Research (IMR) Nordnesgaten 50 Bergen, Norway
C2 CRO, CÔTE D’IVOIRE
   UNIV FELIX HOUPHOUET-BOIGNY, CÔTE D’IVOIRE
   UNIV FELIX HOUPHOUET-BOIGNY, CÔTE D’IVOIRE
   IRD, FRANCE
   IMR (BERGEN), NORWAY
SI BREST
SE IRD
UM LEMAR
TC 0
UR https://archimer.ifremer.fr/doc/00684/79619/82344.pdf
LA English
DT Article
CR CITHER 1 (LEGS 1 ET 2)
   EGEE
   EGEE/1
   EGEE/2
   EGEE/3
   EGEE/4
   EGEE/5
   EGEE/6
   EQUALANT
   EQUALANT 2000
   EQUALANT 99
   FOCAL 2
   FOCAL 4
   FOCAL 6
   FOCAL 7
   FOCAL 8
   GATE PHASE 2
   GATE PHASE 2
   PICOLO P5
   PIRATA
   PIRATA FR24
   PIRATA FR25
   PIRATA FR26
   PIRATA FR27
   PIRATA-FR06
   PIRATA-FR08
   PIRATA-FR09
   PIRATA-FR10
   PIRATA-FR11
   PIRATA-FR12
   PIRATA-FR18
   PIRATA-FR19
   PIRATA-FR2
   PIRATA-FR20
   PIRATA-FR22 LEG1
   PIRATA-FR22 LEG2
   PIRATA-FR23 LEG1
   PIRATA-FR3
   PIRATA-FR5
   RECIF CAP 7314 NANSEN
   SUPREA
BO L'Atalante
   Le Suroît
   Antea
   Thalassa
   Capricorne
   Perle
DE ;Atlantic Ocean;Gulf of Guinea;Mixed Layer;Spatial Variability;Seasonal Variability.
AB The spatial and seasonal variability of the mixed layer depth (MLD) was studied using hydrological data from several databases collected over the period October 1973 to March 2017 at 10 °W between latitudes 2 °N and 10 °S in the Gulf of Guinea. The density threshold method with 0.03 kg m-3 criterion was used to calculate the MLD. In the equatorial band, the seasonal average MLD is 20 m whatever the season. At 6 °S and 10 °S, the MLD is relatively higher during the cold season. The MLD varies between 21 and 37 m at 6 °S, and the seasonal averages MLD are 21 and 40 m respectively during the hot and cold seasons. At 10 °S, during the hot season, the MLD varies between 28 and 52 m and the seasonal average is 39.5 m. During the cold season, the MLD varies between 45 and 55 m with a seasonal average of 49 m. 
PY 2021
SO European Journal of Scientific Research / Revue Européenne de la recherche Scientifique
SN 1450-216X / 1450-202
PU FRDN Incorporated
VL 158
IS 3
BP 207
EP 217
ID 79619
ER

EF