North Atlantic Ocean surface currents

By G. Reverdin, P. Niiler, H. Valdimarsson. 2003

214 citations recorded by the source corpus.

Subfields: Global and Planetary Change, Oceanography

View Paper: https://www.semanticscholar.org/paper/6034518375ed1f3456ad44534d7e68d41217b422

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. J. Runge
2. F. Hernandez
3. B. Galperin
4. P. Pepin
5. Brian Knights
6. Michael J. Miller
7. B. Niehoff
8. Ricardo S. Santos

In Oceanography

1. D. Chambers
2. M. Heath
3. J. Runge
4. B. Niehoff
5. F. Hernandez
6. P. Pepin
7. J. Pierson
8. Victor Zlotnicki

Citations in the corpus

• The North Atlantic Ocean as habitat for Calanus finmarchicus: Environmental factors and life history traits (2014, methodology): “…statistical and numerical techniques, such as generalised linear models (GLM) and geographic information systems (GIS), have been applied to quantify species distributions, in species distribution models (Elith and Leathwick, 2009), habitat distribution models (Guisan and Zimmermann, 2000) and…”
• Diversity, distribution and spatial structure of the cold-water coral fauna of the Azores (NE Atlantic) (2013, background): “One additional eastward flow can be traced between the 15 NAC and the AzC at 39–42 • N (Reverdin et al., 2003).”
• Oceanic changes in the Sargasso Sea and declines in recruitment of the European eel (2007, background): “The flow structure in the southwestern Sargasso, through which anguillid leptocephali must pass to enter the Florida Current, is complex, but the Antilles Current northeast of the northern Bahamas appears to be present throughout most of the year (Amos et al., 1971; Ingham, 1975; Gunn and Watts, 198”
• Mean Dynamic Topography of the Ocean Derived from Satellite and Drifting Buoy Data Using Three Different Techniques (2009, background): “These observations made it possible to compute significant time-mean currents at mesoscale resolution in the North Atlantic, where the data were sufficiently dense (Reverdin et al. 2003).”
• A mean dynamic topography computed over the world ocean from altimetry, in situ measurements, and a geoid model (2004, methodology): “At 63� W the current bifurcates north and widens and its velocity decreases as already observed by Fratantoni [2001] and Reverdin et al. [2003] .”