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- Fast and slow ocean thermal, carbon and nutrient responses to atmospheric forcing
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- Climate responses after net zero is reached
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- The Role of Mesoscale Eddy Stirring and Microscale Turbulence in Sustaining Biological Production in the Subtropical Gyres
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- Local versus far-field control on South Pacific Subantarctic mode water variability
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- Climate Feedbacks Derived From Spatial Gradients in Recent Climatology
- Sources, Pathways, and Drivers of Sub‐Antarctic Mode Water Formation
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- A normalised framework for the Zero Emissions Commitment
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- North Atlantic Carbon Uptake and Variability: The Gulf Stream's Role in Air-Sea CO2 Flux and Storage
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- A normalised framework for the Zero Emission Commitment: competing controls by thermal and carbon processes
- Understanding the Mechanisms Behind Zero Emissions Commitment (ZEC) at Different Warming Levels
- Contrasting fast and slow ocean carbon and thermal responses to the North Atlantic Oscillation
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- Reinforcing fast and slow carbon responses to atmospheric events in the subpolar North Atlantic 
- Role of Ocean Memory in Subpolar North Atlantic Decadal Variability
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- Surface forcing controls on the volume and heat content of subtropical and subpolar mode waters over the global ocean
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- Climate feedbacks derived from spatial gradients in recent climatology
- Local versus farfield control on South Pacific Subantarctic mode water variability
- Supplementary material to "Local versus farfield control on South Pacific Subantarctic mode water variability"
- An Ocean Memory Perspective: Disentangling Atmospheric Control of Decadal Variability in the North Atlantic Ocean
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- Climate feedbacks derived from theory and spatial contrasts in recent climatology
- An optimal transformation method applied to diagnose the ocean carbon budget
- Historical mismatch in Southern Ocean contribution to global heat and carbon uptake
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- An optimal transformation method applied to diagnosing the ocean carbon sink
- Surface Heat Fluxes Drive a Two‐Phase Response in Southern Ocean Mode Water Stratification
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- On the Arctic Amplification of surface warming in a conceptual climate model
- Climate feedbacks with latitude derived from climatological data and theory
- The role of the Southern Ocean in the global climate response to carbon emissions
- Reconstructing ocean carbon storage with CMIP6 Earth system models and synthetic Argo observations
- Energy budget diagnosis of changing climate feedback
- Lagrangian pathways for heat, carbon and nutrients subdction with sub-Antarctic mode waters
- Fast and slow ocean thermal responses to atmospheric forcing
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- Mechanisms Driving the Dispersal of Hydrothermal Iron From the Northern Mid Atlantic Ridge
- A nutrient relay sustains subtropical ocean productivity
- Impact of negative and positive CO2 emissions on global warming metrics using an ensemble of Earth system model simulations
- Reconstructing ocean carbon storage with CMIP6 models and synthetic Argo observations
- Mechanisms driving the dispersal of hydrothermal iron from the northern Mid Atlantic Ridge
- Subtropical Contribution to Sub‐Antarctic Mode Waters
- Historical Reconstruction of Subpolar North Atlantic Overturning and Its Relationship to Density
- Reconstructing upper ocean carbon variability using ARGO profiles and CMIP6 models
- Identifying the drivers of Subantarctic mode water thickness across the south Pacific.
- Inter-annual Variability in the Subpolar Overturning Circulation: A Sensitivity Analysis
- Ventilation controls of ocean heat and carbon uptake: similarities and differences in the response to carbon emissions
- Subtropical contribution to Subantarctic Mode Waters
- Assessment of negative and positive CO2 emissions on global warming metrics using large ensemble Earth system model simulations
- Supplementary material to "Assessment of negative and positive CO2 emissions on global warming metrics using large ensemble Earth system model simulations"
- Observations of Nutrient Supply by Mesoscale Eddy Stirring and Small‐Scale Turbulence in the Oligotrophic North Atlantic
- Withdrawn: Observations of Nutrient Supply by Mesoscale Eddy Stirring and Diapycnal Mixing in the Oligotrophic North Atlantic
- Ocean carbon cycle feedbacks in CMIP6 models: contributions from different basins
- Regional Asymmetries in Ocean Heat and Carbon Storage due to Dynamic Redistribution in Climate Model Projections
- How does heat flux affect potential vorticity in the Southern Ocean?
- Large ensemble assessment of how the global surface warming response to cumulative carbon differs for negative and positive carbon emissions  
- Added and redistributed heat and carbon in climate model projections for the Southern Ocean
- Controls of the TCRE in Earth system models
- Controls of ocean carbon cycle feedbacks from different ocean basins and meridional overturning in CMIP6
- Internal Tide‐Driven Tracer Transport Across the Continental Slope
- Carbon–concentration and carbon–climate feedbacks in CMIP6 models and their comparison to CMIP5 models
- Resource Availability and Entrainment Are Driven by Offsets Between Nutriclines and Winter Mixed‐Layer Depth
- Why do the latest climate models differ in how much surface warming increases with carbon emissions?
- Carbon-concentration and carbon-climate feedbacks in CMIP6 models, and their comparison to CMIP5 models
- Controls of the Transient Climate Response to Emissions: effects of physical feedbacks, heat uptake and saturation of radiative forcing
- Sensitivity of climate mitigation signals to climate engineering choice and implementation
- Which Processes Sustain Biota in Open-Ocean Deep Chlorophyll Maxima?
- Is there warming in the pipeline? A multi-model analysis of the zero emission commitment from CO2
- Carbon-concentration and carbon-climate feedbacks in CMIP6 models, and their comparison to CMIP5 models
- Supplementary material to "Carbon-concentration and carbon-climate feedbacks in CMIP6 models, and their comparison to CMIP5 models"
- Carbon-Cycle Feedbacks Operating in the Climate System
- Internal Tides Drive Nutrient Fluxes Into the Deep Chlorophyll Maximum Over Mid‐ocean Ridges
- Climate sensitivity from both physical and carbon cycle feedbacks
- Overturning in the subpolar North Atlantic
- Connecting surface warming to carbon emissions - atmospheric and oceanic viewpoints
- How much time is left before we reach global warming targets of 1.5°C or 2°C?
- Sensitivity of global surface warming to carbon emissions in a suite of climate models
- On how surface warming continues after carbon emissions cease
- Overturning in the Subpolar North Atlantic Program: A New International Ocean Observing System
- Variations in the difference between mean sea level measured either side of Cape Hatteras and their relation to the North Atlantic Oscillation
- Quantifying the drivers of ocean-atmosphere CO2 fluxes
- A new metric defining how the winds and ocean eddies in the Southern Ocean alter atmospheric CO2
- Volcanic ash as an oceanic iron source and sink
- A framework to understand how global surface warming connects to carbon emissions
- How does ocean heat content change over the North Atlantic Ocean?
- Physical controls of variability in North Atlantic phytoplankton communities
- A single equation connecting global surface warming with carbon emissions
- Mean sea-level variability along the northeast American Atlantic coast and the roles of the wind and the overturning circulation
- A ventilation-based framework to explain the regeneration-scavenging balance of iron in the ocean
- Evidence for production and lateral transport of dissolved organic phosphorus in the eastern subtropical North Atlantic
- The impact of fine-scale turbulence on phytoplankton community structure
- How ocean circulation affects the pattern of warming in the North Atlantic Ocean
- The paradox of the plankton: species competition and nutrient feedback sustain phytoplankton diversity
- Water Mass Transformations in the Southern Ocean Diagnosed from Observations: Contrasting Effects of Air–Sea Fluxes and Diapycnal Mixing
- Internal Wave Reflection on Shelf Slopes with Depth-Varying Stratification
- How the winds in the Southern Ocean alter atmospheric CO2 by upwelling of carbon-rich deep waters
- How warming and steric sea level rise relate to cumulative carbon emissions
- Sea level changes at Ascension Island in the last half century
- Oceanography: Centennial warming of ocean jets
- Nutrient streams in the North Atlantic: Advective pathways of inorganic and dissolved organic nutrients
- The supply of excess phosphate across the Gulf Stream and the maintenance of subtropical nitrogen fixation
- Oceanography: Ocean eddies and plankton blooms
- Internal tides, nonlinear internal wave trains, and mixing in the Faroe-Shetland Channel
- The shaping of storm tracks by mountains and ocean dynamics
- Opposing decadal changes for the North Atlantic meridional overturning circulation
- Opposing decadal changes for the North Atlantic meridional overturning circulation
- Modelling the effects of chromatic adaptation on phytoplankton community structure in the oligotrophic ocean
- Water-mass transformation in the shelf seas
- On the Buoyancy Forcing and Residual Circulation in the Southern Ocean: The Feedback from Ekman and Eddy Transfer
- Distribution of dissolved organic nutrients and their effect on export production over the Atlantic Ocean
- Are mesoscale eddies in shelf seas formed by baroclinic instability of tidal fronts?
- The Effect of Ocean Dynamics and Orography on Atmospheric Storm Tracks
- Climate sensitivity to the carbon cycle modulated by past and future changes in ocean chemistry
- Ocean dynamics and the carbon cycle (ISBN 978-0-521-84369-0)
- Analytical relationships between atmospheric carbon dioxide, carbon emissions, and ocean processes
- Boundary wave communication of bottom pressure and overturning changes for the North Atlantic
- Phosphorus cycling in the North and South Atlantic Ocean subtropical gyres
- The Spatial Pattern and Mechanisms of Heat-Content Change in the North Atlantic
- Meridional coherence of the North Atlantic meridional overturning circulation
- How widespread and important is N2fixation in the North Atlantic Ocean?
- Ocean and Atmosphere Storm Tracks: The Role of Eddy Vorticity Forcing
- A twenty year reversal in water mass trends in the subtropical North Atlantic
- Ocean-atmosphere partitioning of anthropogenic carbon dioxide on centennial timescales
- Topographic Control of Basin and Channel Flows: The Role of Bottom Pressure Torques and Friction
- Does the transport of dissolved organic nutrients affect export production in the Atlantic Ocean?
- The Atlantic Meridional Transect (AMT) Programme: A contextual view 1995–2005
- Nutrient streams and their induction into the mixed layer
- When Are Eddy Tracer Fluxes Directed Downgradient?
- Role of bottom water transport and diapycnic mixing in determining the radiocarbon distribution in the Pacific
- The Role of Sloping Sidewalls in Forming Potential Vorticity Contrasts in the Ocean Interior
- Comparing the overflow of dense water in isopycnic and cartesian models with tracer observations in the eastern Mediterranean
- Estimating the convective supply of nitrate and implied variability in export production over the North Atlantic
- The role of eddies in the isopycnic transfer of nutrients and their impact on biological production
- Impact of the circulation on Sapropel Formation in the eastern Mediterranean
- Estimating climatological age from a model-derived oxygen–age relationship in the Mediterranean
- Oceanography: Eddies make ocean deserts bloom
- The Ekman transfer of nutrients and maintenance of new production over the North Atlantic
- Inferring the Subduction Rate and Period over the North Atlantic
- Cooling Parsons’ Model of the Separated Gulf Stream
- The Influence of Air–Sea Interaction on the Ventilated Thermocline
- Modification of ocean eddies by air-sea interaction