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Deep Circulation in the South Atlantic Induced by Bottom-Intensified Mixing over the Midocean Ridge in: Journal of Physical Oceanography Volume 32 Issue 4 (2002)
Frontiers Three-dimensional numerical study of the deep western boundary current in the South China Sea
As for the previous figure except in neutral density space calculated
Deep-Sea Symphony: Exploring the Musicians Seamounts: Background: Biogeography of Pacific Islands and Seamounts: NOAA Office of Ocean Exploration and Research
Frontiers Three-dimensional numerical study of the deep western boundary current in the South China Sea
South China Sea documents the transition from wide continental rift to continental break up
Deep Circulation in the South Atlantic Induced by Bottom-Intensified Mixing over the Midocean Ridge in: Journal of Physical Oceanography Volume 32 Issue 4 (2002)
PDF) Ocean Dynamics and Topographic Upwelling Around the Aracati Seamount - North Brazilian Chain From in situ Observations and Modeling Results
Deep Circulation in the South Atlantic Induced by Bottom-Intensified Mixing over the Midocean Ridge in: Journal of Physical Oceanography Volume 32 Issue 4 (2002)
Overview of the ChinStrAP (Changes in Stratification at the Antarctic