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Observed and simulated variability of the AMOC at 26°N and 41°N
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Observed and simulated variability of the AMOC at 26°N and 41°N
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Regional and temporal evolution of sea-surface pCO2 in Arctic waters
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Observed and simulated variability of the AMOC at 26 degrees N and 41 degrees N
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Coherent Circulation Changes in the Deep North Atlantic From 16°N and 26°N Trans...
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Coherent changes of the circulation in the deep North Atlantic from moored trans...
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Horizontal Stratification during Deep Convection in the Labrador Sea
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Coherent circulation changes in the deep North Atlantic from 16N and 26N transpo...
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Coherent changes of the circulation in the deep North Atlantic from moored trans...
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Observed basin-scale response of the North Atlantic meridional overturning circu...
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Vertical structure of eddies and Rossby waves, and their effect on the Atlantic...
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Vertical structure of eddies and Rossby waves, and their effect on the Atlantic...
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Variability of Antarctic bottom water at 24.5 degrees N in the Atlantic
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Detectability of an AMOC decline in current and projected climate changes
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Detectability of an AMOC decline in current and projected climate changes
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Variability of Antarctic Bottom Water at 24.5°N in the Atlantic
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Vertical structure of eddies and Rossby waves, and their effect on the Atlantic...
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Variability of Antarctic Bottom Water at 24.5°N in the Atlantic
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Determining Vertical Water Velocities from Seaglider
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Determining vertical water velocities from Seaglider
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