Atmospheric Moisture Transport Moderates Climatic Response to the Opening of Drake Passage

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CORRIGENDUM

Can Isopycnal Mixing Control the Stability of the Thermohaline Circulation in Ocean Climate Models?

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Changes in ocean vertical heat transport with global warming

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Corrigendum to “The effect of a northward shift in the southern hemisphere westerlies on the global ocean” [Prog Oceanogr 79 (2008) 1–19]

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Effect of Ocean Gateway Changes under Greenhouse Warmth

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Effect of the deepening of the Tasman Gateway on the global ocean

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Ice–Atmosphere Feedbacks Dominate the Response of the Climate System to Drake Passage Closure

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Model simulations of early westward flow across the Tasman Gateway during the early Eocene

North Atlantic Climate Response to Lake Agassiz Drainage at Coarse and Ocean Eddy-Permitting Resolutions

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Precise Calculations of the Existence of Multiple AMOC Equilibria in Coupled Climate Models. Part I: Equilibrium States

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Precise Calculations of the Existence of Multiple AMOC Equilibria in Coupled Climate Models. Part II: Transient Behavior

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Pronounced zonal heterogeneity in Eocene southern high-latitude sea surface temperatures

scientific article (publication date: 6 May 2014)

Reduced Stability of the Atlantic Meridional Overturning Circulation due to Wind Stress Feedback during Glacial Times

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Revisiting meridional overturing bistability using a minimal set of state variables: stochastic theory

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Role of the Drake Passage in Controlling the Stability of the Ocean’s Thermohaline Circulation

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Sensitivity of the Atlantic Thermohaline Circulation and Its Stability to Basin-Scale Variations in Vertical Mixing

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Southern Hemisphere Westerly Wind Control over the Ocean's Thermohaline Circulation

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Stability of Antarctic Bottom Water Formation to Freshwater Fluxes and Implications for Global Climate

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The Control of Polar Haloclines by Along-Isopycnal Diffusion in Climate Models

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The Key Role of the Western Boundary in Linking the AMOC Strength to the North–South Pressure Gradient

scientific article published in 2012

The Ocean Circulation in Thermohaline Coordinates

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The Role of Bottom Pressure Torques on the Interior Pathways of North Atlantic Deep Water

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The effect of a northward shift in the southern hemisphere westerlies on the global ocean

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The effect of low ancient greenhouse climate temperature gradients on the ocean's overturning circulation

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The role of carbon dioxide during the onset of Antarctic glaciation

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The role of ocean gateways on cooling climate on long time scales

scholarly article by Willem Sijp published in August 2014

Vertical Heat Transport by Ocean Circulation and the Role of Mechanical and Haline Forcing

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