Near-surface circulation in the Tropical Atlantic Ocean

By R. Lumpkin, S. Garzoli. 2005

233 citations recorded by the source corpus.

Subfields: Global and Planetary Change, Oceanography

View Paper: https://www.semanticscholar.org/paper/b5e61331bfe0a39e8310c69f61ffb1dabe013360

How researchers see this paper

The researchers whose trusted networks rank it highest, strongest advocate first. Every researcher gets a different order.

In Global and Planetary Change

1. F. Hernandez
2. Maureen T. Brooks
3. R. Lumpkin
4. Chuanmin Hu
5. F. Werner
6. N. Putman
7. M. Mcphaden
8. S. Planton

In Oceanography

1. F. Hernandez
2. Maureen T. Brooks
3. R. Lumpkin
4. Chuanmin Hu
5. F. Werner
6. N. Putman
7. M. Mcphaden
8. S. Planton

Citations in the corpus

• Lagrangian Analysis and Prediction of Coastal and Ocean Dynamics: Measuring surface currents with Surface Velocity Program drifters: the instrument, its data, and some recent results (2007, background): “The array spanned the tropical and South Atlantic Ocean by 2004 ( Lumpkin and Garzoli, 2005 ).”
• Tropical Atlantic biases and their relation to surface wind stress and terrestrial precipitation (2012, unknown): “2c; Lumpkin and Garzoli 2005).”
• ORIGINAL ARTICLE: Freshwater paths across the ocean: molecular phylogeny of the frog Ptychadena newtoni gives insights into amphibian colonization of oceanic islands (2006, unknown): “Journal compilation ª 2006 Blackwell Publishing Ltd hydrographical data, and surface-drifting buoy trajectories (Richardson & Walsh, 1986; Arnault, 1987; Stramma & Schott, 1999; Lumpkin & Garzoli, 2005).”
• THE PIRATA PROGRAM History, Accomplishments, and Future Directions * (2008, background): “The equatorial Atlantic exhibits a complex system of zonal currents at different depths and latitudes, along with areas of upwelling (upward flow) and subduction (downward flow) (e.g., Bourles et al. 2002; Stramma et al. 2003; Schott et al. 2004; Lumpkin and Garzoli 2005; Fig.”
• The establishment of a pelagic Sargassum population in the tropical Atlantic: Biological consequences of a basin-scale long distance dispersal event (2020, background): “Every May, the North Equatorial Counter Current (NECC) forms, and the NBC separates from the coast, retroflects, and flows eastward, joining the NECC (Muller-Karger et al., 1988, 1995; Richardson et al., 1992; Lumpkin and Garzoli, 2005).”