The large-scale time-mean ocean circulation in the Nordic Seas and Arctic Ocean estimated from simplified dynamics
By O. Nøst, P. Isachsen. 2003
178 citations recorded by the source corpus.
Subfields: Atmospheric Science, Global and Planetary Change, Oceanography
View Paper: https://www.semanticscholar.org/paper/5b50e7ddb538eb18183992536331c6e9b4b2e864
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In Atmospheric Science
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In Oceanography
Citations in the corpus
- At the rainbow’s end: high productivity fueled by winter upwelling along an Arctic shelf (2014, background): “The density gradient between the relatively light Arctic and denser Atlantic Water generally prevents upwelling of the latter (Nansen 1902; Rudels et al. 1999).”
- Eddy‐driven recirculation of Atlantic Water in Fram Strait (2016, background): “It is known that currents have a strong barotropic component in this weakly stratified high-latitude region and thus approximately follow the bottom topography or, more precisely, f/H contours, where f is the Coriolis parameter and H the water depth [Isachsen et al., 2003; Nøst and Isachsen, 2003].”