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An analytical model of open-ocean deep convection with multiple steady states
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The Spatio-Temporal Variability of the Ocean-Atmosphere Heat Exchange and the Se...
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Formation and decay of a deep convective chimney
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Properties and pathways of Mediterranean water eddies in the Atlantic
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Properties and pathways of Mediterranean water eddies in the Atlantic
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Properties and pathways of Mediterranean water eddies in the Atlantic
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The influence of the North Atlantic Oscillation on the abundance of Pagellus bog...
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The influence of the North Atlantic Oscillation on the abundance of Pagellus bog...
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Application of the theory of columnar Q-vortices with helical structure for the...
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Accuracy assessment of primary production models with and without photoinhibitio...
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Intra-annual and interannual non-stationary cycles of chlorophyll concentration...
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An Influence of Meridional Oceanic and Atmospheric Heat Fluxes to the Atlantic S...
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Distribution of intermediate water masses in the subtropical northeast Atlantic
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Distribution of intermediate water masses in the subtropical northeast Atlantic
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Distribution of intermediate water masses in the subtropical northeast Atlantic
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Sea ice volume variability and water temperature in the Greenland Sea
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Mediterranean outflow transports and entrainment estimates from observations and...
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Mediterranean outflow transports and entrainment estimates from observations and...
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Mediterranean outflow transports and entrainment estimates from observations and...
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Mediterranean outflow transports and entrainment estimates from observations and...
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Entrainment of 1.1 Sv NACW from Lagrangian analysis in closed domain in GoC
MU velocity veins and thermohaline anomaly cores are not co-located
Most of NACW entrained comes from south and southwest borders
Westward salinity and heat transports are of ∼1.3 psu Sv and ∼20 × 1012 W
Westward volume transport is 2.6–3.6 Sv in observations and 3.5 Sv in model
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