All Stories
- Why do the latest climate models differ in how much surface warming increases with carbon emissions?
Article
- Carbon-concentration and carbon-climate feedbacks in CMIP6 models, and their comparison to CMIP5 models
Article
- Supplementary material to "Carbon-concentration and carbon-climate feedbacks in CMIP6 models, and their comparison to CMIP5 models"
Article
- Carbon-Cycle Feedbacks Operating in the Climate System
Article
- 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
Article
- Connecting surface warming to carbon emissions - atmospheric and oceanic viewpoints
Article
- 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
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- On how surface warming continues after carbon emissions cease
Article
- Overturning in the Subpolar North Atlantic Program: A New International Ocean Observing System
Article
- 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
Article
- 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