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