![]() Garzoli, Deep Western Boundary Current transport variability in the South Atlantic: Preliminary results from a pilot array at 34.5°S, Ocean Sci., 8, 1041-1054, doi:10.5194/os-8-1041-2012, 2012. NOAA, USP, SHN, UCT/DEA, ENS/IFREMER / 2020 (2018) publicationĪs it contains the appropriate credit for all of the data producers in the Acknowledgements. If you use data from SAMBA, please make sure to cite the Meinen et al. Is made freely available to the public at: MOC transport data from the South Atlantic MOC Basin-wide Array (SAMBA) These data are freely available via the web page." Ocean Observation and Monitoring Division and the Atlantic Oceanographic and Meteorological Laboratory. "Data from the Southwest Atlantic MOC project (SAM) are funded by the DOC-NOAA Climate Program Office. Project scientists would appreciate it if you added the following acknowledgment to any publications that use these data: The raw NOAA PIES data have been archived at NOAA NCEI.ĭata for the other individual instruments in SAMBA can be obtained by request from the lead scientists within each participating country.ĭata from the Southwest Atlantic MOC project are made freely available to the public. The continuous travel time and bottom pressure data from the individual NOAA PIES instruments in the western array are also availableĪs is a subset of the western boundary hydrography data. (2013) paper can also be downloaded from the “Data Access” page at: Meridional overturning circulation transport variability at 34.5°S during 2009–2017:īaroclinic and barotropic flows and the dueling influence of the boundaries. Transport data (Note that different from the other TMAs these are transport anomalies!) can be downloaded here ![]() Was calculated holding the bottom pressure values on both sides of the basin constant).įrom Meinen et al., GRL, 2018, doi: 10.1029/2018GL077408. (i.e., the reference contribution is the difference between the total MOC and the MOC that The geostrophic relative and reference flow components are further broken down into the contributionsįrom variations in the western and eastern density or pressure contributions, respectively.įor all components, the “contribution” is estimated as the difference between the total MOC (black line)Īnd the MOC calculated while holding the term in question constant The record‐length mean total MOC value that has been removed to create the anomaly is noted on the figure.Īlso shown are the contributions of Ekman, geostrophic reference flow, and geostrophic relative flow components The total (net) transport anomaly is shown in black. 2: Time series (temporal anomaly relative to the record‐length mean) of the basin‐wide MOC volume transport across 34.5°S. AOMLĪlberto Piola, hydrography-west, Meinen, PIES-west, Campos, CPIES-west, Speich, CPIES-east, Ansorge, moored V, T, S, hydrography-east, products: volume transport time seriesįig. USA: NOAA-Atlantic Oceanographic and Meteorological Lab. South Africa: University of Cape Town UCT & Dept. of Buenos Aires UBAįrance: Ecole Normale Superieure, ENS & IFREMER, Univ. SAMBA South Atlantic Meridional Overturning Circulation – Basin-wide ArrayĪrgentina: Servicio de Hidrografia Naval SHN & Univ. SAMBA-SAMOC South Atlantic Meridional Overturning Circulation MOVE Meridional Overturning Variability ExperimentĨ. ![]() RAPID-MOCHA-WBTS Rapid Climate Change Meridional Overturning Circulation Heat-flux ArrayĦ. OSNAP Overturning in the Subpolar North Atlantic Programĥ.
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