FN Archimer Export Format
PT C
TI Oceanic Circulation in the Strait of Gibraltar revealed by AIS data Information
BT 
AF Le Goff, C
   Mironov, AS
   Boussidi, B
   Bordois, L
   Dumas, F
   CHAPRON, Bertrand
AS 1:1;2:1;3:1;4:2;5:2;6:3;
FF 1:;2:;3:;4:;5:;6:PDG-ODE-LOPS-SIAM;
C1 e-odyn, Brest, France
   SHOM, Brest, France
   Laboratory for Ocean Physics and Satellite Remote Sensing, Ifremer Brest, France
C2 E-ODYN, FRANCE
   SHOM, FRANCE
   IFREMER, FRANCE
SI BREST
SE PDG-ODE-LOPS-SIAM
UM LOPS
UR https://archimer.ifremer.fr/doc/00693/80508/83719.pdf
LA English
DT Proceedings paper
CR PROTEVS 2020
BO L'Atalante
DE ;AIS;Oceanic Surface Current;Drift speed;Tides
AB Our understanding of ocean circulation to date still bears many unanswered questions. Despite the development of a variety of methods for observing upper ocean current velocity at different scales, our knowledge of this subject has yet to be significantly improved. Historically, the drift of vessels led to the discovery of the oceanic surface current. The Automatic Identification System (AIS), originally intended to avoid collision in maritime traffic, contains the necessary information to retrieve vessel drift due to the surface current. Thus, the AIS data can be processed to derive sea-surface current components for any region in which there is maritime traffic. A dedicated inversion scheme has recently been theoretically formulated and implemented. In this study, we report the preliminary results obtained during an experimental campaign conducted aboard the oceanographic vessel Atalante, in the strait of Gibraltar, in October 2020. A map of oceanic circulation was calculated using the drift of all vessels emitting AIS messages within the strait and validation was achieved with the help of an Acoustic Doppler current profiler (ADCP) aboard the Atalante. 
PY 2021
CT IGARSS 2021. 12-14 July 2021, Brussels. Session WE1.O-9 "Remote Sensing of Ocean Currents", ISBN:978-1-6654-4762-1, Paper WE1.O-9.6. pp. 7358-7361
DI 10.1109/IGARSS47720.2021.9554044
ID 80508
ER

EF