All Stories
- Historical mismatch in Southern Ocean contribution to global heat and carbon uptake
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- Why do the latest climate models differ in how much surface warming increases with carbon emissions?
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- Carbon-concentration and carbon-climate feedbacks in CMIP6 models, and their comparison to CMIP5 models
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- Supplementary material to "Carbon-concentration and carbon-climate feedbacks in CMIP6 models, and their comparison to CMIP5 models"
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- Carbon-Cycle Feedbacks Operating in the Climate System
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- Internal Tides Drive Nutrient Fluxes Into the Deep Chlorophyll Maximum Over Mid‐ocean Ridges
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- Climate sensitivity from both physical and carbon cycle feedbacks
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- Overturning in the subpolar North Atlantic
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- Connecting surface warming to carbon emissions - atmospheric and oceanic viewpoints
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- How much time is left before we reach global warming targets of 1.5°C or 2°C?
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- Sensitivity of global surface warming to carbon emissions in a suite of climate models
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- On how surface warming continues after carbon emissions cease
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- Overturning in the Subpolar North Atlantic Program: A New International Ocean Observing System
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- Variations in the difference between mean sea level measured either side of Cape Hatteras and their relation to the North Atlantic Oscillation
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- Quantifying the drivers of ocean-atmosphere CO2 fluxes
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- A new metric defining how the winds and ocean eddies in the Southern Ocean alter atmospheric CO2
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- Volcanic ash as an oceanic iron source and sink
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- A framework to understand how global surface warming connects to carbon emissions
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- How does ocean heat content change over the North Atlantic Ocean?
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- Physical controls of variability in North Atlantic phytoplankton communities
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- A single equation connecting global surface warming with carbon emissions
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- Mean sea-level variability along the northeast American Atlantic coast and the roles of the wind and the overturning circulation
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- A ventilation-based framework to explain the regeneration-scavenging balance of iron in the ocean
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- Evidence for production and lateral transport of dissolved organic phosphorus in the eastern subtropical North Atlantic
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- The impact of fine-scale turbulence on phytoplankton community structure
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- How ocean circulation affects the pattern of warming in the North Atlantic Ocean
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- The paradox of the plankton: species competition and nutrient feedback sustain phytoplankton diversity
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- Water Mass Transformations in the Southern Ocean Diagnosed from Observations: Contrasting Effects of Air–Sea Fluxes and Diapycnal Mixing
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- Internal Wave Reflection on Shelf Slopes with Depth-Varying Stratification
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- How the winds in the Southern Ocean alter atmospheric CO2 by upwelling of carbon-rich deep waters
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- How warming and steric sea level rise relate to cumulative carbon emissions
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- Sea level changes at Ascension Island in the last half century
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- Oceanography: Centennial warming of ocean jets
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- Nutrient streams in the North Atlantic: Advective pathways of inorganic and dissolved organic nutrients
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- The supply of excess phosphate across the Gulf Stream and the maintenance of subtropical nitrogen fixation
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- Oceanography: Ocean eddies and plankton blooms
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- Internal tides, nonlinear internal wave trains, and mixing in the Faroe-Shetland Channel
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- The shaping of storm tracks by mountains and ocean dynamics
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- Opposing decadal changes for the North Atlantic meridional overturning circulation
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- Opposing decadal changes for the North Atlantic meridional overturning circulation
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- Modelling the effects of chromatic adaptation on phytoplankton community structure in the oligotrophic ocean
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- Water-mass transformation in the shelf seas
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- On the Buoyancy Forcing and Residual Circulation in the Southern Ocean: The Feedback from Ekman and Eddy Transfer
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- Distribution of dissolved organic nutrients and their effect on export production over the Atlantic Ocean
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- Are mesoscale eddies in shelf seas formed by baroclinic instability of tidal fronts?
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- The Effect of Ocean Dynamics and Orography on Atmospheric Storm Tracks
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- Climate sensitivity to the carbon cycle modulated by past and future changes in ocean chemistry
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- Ocean dynamics and the carbon cycle (ISBN 978-0-521-84369-0)
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- Analytical relationships between atmospheric carbon dioxide, carbon emissions, and ocean processes
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- Boundary wave communication of bottom pressure and overturning changes for the North Atlantic
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- Phosphorus cycling in the North and South Atlantic Ocean subtropical gyres
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- The Spatial Pattern and Mechanisms of Heat-Content Change in the North Atlantic
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- Meridional coherence of the North Atlantic meridional overturning circulation
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- How widespread and important is N2fixation in the North Atlantic Ocean?
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- Ocean and Atmosphere Storm Tracks: The Role of Eddy Vorticity Forcing
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- A twenty year reversal in water mass trends in the subtropical North Atlantic
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- Ocean-atmosphere partitioning of anthropogenic carbon dioxide on centennial timescales
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- Topographic Control of Basin and Channel Flows: The Role of Bottom Pressure Torques and Friction
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- Does the transport of dissolved organic nutrients affect export production in the Atlantic Ocean?
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- The Atlantic Meridional Transect (AMT) Programme: A contextual view 1995–2005
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- Nutrient streams and their induction into the mixed layer
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- When Are Eddy Tracer Fluxes Directed Downgradient?
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- Role of bottom water transport and diapycnic mixing in determining the radiocarbon distribution in the Pacific
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- The Role of Sloping Sidewalls in Forming Potential Vorticity Contrasts in the Ocean Interior
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- Comparing the overflow of dense water in isopycnic and cartesian models with tracer observations in the eastern Mediterranean
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- Estimating the convective supply of nitrate and implied variability in export production over the North Atlantic
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- The role of eddies in the isopycnic transfer of nutrients and their impact on biological production
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- Impact of the circulation on Sapropel Formation in the eastern Mediterranean
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- Estimating climatological age from a model-derived oxygen–age relationship in the Mediterranean
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- Oceanography: Eddies make ocean deserts bloom
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- The Ekman transfer of nutrients and maintenance of new production over the North Atlantic
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- Inferring the Subduction Rate and Period over the North Atlantic
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- Cooling Parsons’ Model of the Separated Gulf Stream
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- The Influence of Air–Sea Interaction on the Ventilated Thermocline
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- Modification of ocean eddies by air-sea interaction
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