This is an appendix to: The Saturation Chronicles - 24
Comments on the references are in brackets[]; e.g. "[TEOS-10 does not appear]"
Global Warming of 1.5°C (2022) [TEOS-10 does not appear]; Warming caused by cumulative carbon emissions towards the trillionth tonne (2009) [TEOS-10 did not apply before 2010]; Southern Ocean warming delayed by circumpolar upwelling and equatorward transport (2016) [TEOS-10 does not appear]; Sea-surface temperature pattern effects have slowed global warming and biased warming-based constraints on climate sensitivity (2024) [TEOS-10 does not appear]; Carbon–concentration and carbon–climate feedbacks in CMIP6 models and their comparison to CMIP5 models (2020) [TEOS-10 does not appear]; Baroclinic Control of Southern Ocean Eddy Upwelling Near Topography (2022) [TEOS-10 does not appear]; Response of the Ocean Natural Carbon Storage to Projected Twenty-First-Century Climate Change (2014) [TEOS-10 does not appear]; Stratification constrains future heat and carbon uptake in the Southern Ocean between 30°S and 55°S (2022) [TEOS-10 was referenced]; Toward quantifying the response of the oceans' biological pump to climate change (2015) [TEOS-10 does not appear]; Heat and carbon coupling reveals ocean warming due to circulation changes (2020) [TEOS-10 does not appear]; Antarctic offshore polynyas linked to Southern Hemisphere climate anomalies (2019) [TEOS-10 does not appear]; Microwave Observation of the Weddell Polynya (1980)[TEOS-10 did not apply before 2010]; Preformed Properties for Marine Organic Matter and Carbonate Mineral Cycling Quantification (2020) [TEOS-10 does not appear]; Preformed Properties for Marine Organic Matter and Carbonate Mineral Cycling Quantification (2020) [TEOS-10 does not appear]; The Southern Ocean as the climate's freight train – driving ongoing global warming under zero-emission scenarios with ACCESS-ESM1.5 (2024) [TEOS-10 does not appear]; The Deep Ocean's Carbon Exhaust (2022) [TEOS-10 was referenced]; Reduced Deep Convection and Bottom Water Formation Due To Antarctic Meltwater in a Multi-Model Ensemble (2023) [TEOS-10 does not appear]; What goes in must come out: the oceanic outgassing of anthropogenic carbon (2024) [TEOS-10 does not appear]; Cessation of deep convection in the open Southern Ocean under anthropogenic climate change (2014) [TEOS-10 does not appear]; The Ocean Carbon Cycle (2022) [TEOS-10 does not appear]; Shortwave and longwave radiative contributions to global warming under increasing CO2 (2014) [TEOS-10 does not appear]; Preconditioning of the Weddell Sea Polynya by the Ocean Mesoscale and Dense Water Overflows (2017) [TEOS-10 does not appear]; Physical Mechanisms Driving Enhanced Carbon Sequestration by the Biological Pump Under Climate Warming (2023) [TEOS-10 does not appear]; Heat and carbon coupling reveals ocean warming due to circulation changes (2020) [TEOS-10 does not appear]; Antarctic offshore polynyas linked to Southern Hemisphere climate anomalies (2019) [TEOS-10 does not appear]; Irreversible ocean thermal expansion under carbon dioxide removal (2018) [TEOS-10 does not appear]; The Sensitivity of the Proportionality between Temperature Change and Cumulative CO2 Emissions to Ocean Mixing (2017) [TEOS-10 does not appear]; Sensitivity of the inorganic ocean carbon cycle to future climate warming in the UVic coupled model (2010) [TEOS-10 does not appear]; Misconceptions of the marine biological carbon pump in a changing climate: Thinking outside the “export” box (2024) [TEOS-10 does not appear]; Global Carbon Budget (2022) [TEOS-10 does not appear]; Contrasting Upper and Deep Ocean Oxygen Response to Protracted Global Warming (2020) [TEOS-10 does not appear]; Dominance of the Southern Ocean in Anthropogenic Carbon and Heat Uptake in CMIP5 Models (2015) [TEOS-10 does not appear]; Shutdown of Southern Ocean convection controls long-term greenhouse gas-induced warming (2021) [TEOS-10 does not appear]; Analytical relationships between atmospheric carbon dioxide, carbon emissions, and ocean processes (2008) [TEOS-10 did not apply before 2010]; Southern Ocean polynya (2014) [not searched, not open access]; The Flux-Anomaly-Forced Model Intercomparison Project (FAFMIP) contribution to CMIP6: investigation of sea-level and ocean climate change in response to CO2 forcing (2016) [TEOS-10 does not appear]; Trends and variability in the ocean carbon sink (2023) [TEOS-10 does not appear]; Oceanic sources, sinks, and transport of atmospheric CO2 (2009) [TEOS-10 did not apply before 2010]; Recent reduced abyssal overturning and ventilation in the Australian Antarctic Basin (2023) [TEOS-10 was referenced]; Sea-Ice Induced Southern Ocean Subsurface Warming and Surface Cooling in a Warming Climate (2020) [TEOS-10 does not appear]; Antarctic Bottom Water and North Atlantic Deep Water in CMIP6 models (2021) [TEOS-10 does not appear]; Increasing vertical mixing to reduce Southern Ocean deep convection in NEMO3.4 (2015) [TEOS-10 does not appear]; Atlantic Ocean Heat Transport Enabled by Indo-Pacific Heat Uptake and Mixing (2019) [TEOS-10 does not appear]; Drivers and distribution of global ocean heat uptake over the last half century (2022) [TEOS-10 was referenced]; Preformed phosphate, soft tissue pump and atmospheric CO2 (2005) [TEOS-10 did not apply before 2010]; Control of Lower-Limb Overturning Circulation in the Southern Ocean by Diapycnal Mixing and Mesoscale Eddy Transfer (2008) [TEOS-10 did not apply before 2010]; Spatial and seasonal variability of the air-sea equilibration timescale of carbon dioxide (2014) [TEOS-10 does not appear]; The Effects of Carbon Dioxide Removal on the Carbon Cycle (2018) [TEOS-10 does not appear]; The Carbon Dioxide Removal Model Intercomparison Project (CDRMIP): rationale and experimental protocol for CMIP6 (2018) [TEOS-10 does not appear]; A new marine ecosystem model for the University of Victoria Earth System Climate Model (2012) [TEOS-10 does not appear]; Air-sea disequilibrium enhances ocean carbon storage during glacial periods (2019) [TEOS-10 does not appear]; Supplemental data (2025) [TEOS-10 does not appear]; Oxygen utilization rate (OUR) underestimates ocean respiration: A model study (2016) [TEOS-10 does not appear]; Does Export Production Measure Transient Changes of the Biological Carbon Pump's Feedback to the Atmosphere Under Global Warming? (2020) [TEOS-10 does not appear]; Marine carbon sink dominated by biological pump after temperature overshoot (2024) [TEOS-10 does not appear]; Asymmetric dynamical ocean responses in warming icehouse and cooling greenhouse climates (2018) [TEOS-10 does not appear]; Abyssal ocean overturning slowdown and warming driven by Antarctic meltwater (2023) [TEOS-10 does not appear]; Global Ocean Meridional Overturning (2007) [TEOS-10 did not apply before 2010]; The Transient Response to Cumulative CO2 Emissions: a Review (2015) [TEOS-10 does not appear]; The oceanic origin of path-independent carbon budgets (2017) [TEOS-10 does not appear]; Closure of the meridional overturning circulation through Southern Ocean upwelling (2012) [TEOS-10 does not appear]; Multi-centennial variability controlled by Southern Ocean convection in the Kiel Climate Model (2012) [TEOS-10 does not appear]; The proportionality of global warming to cumulative carbon emissions (2009) [TEOS-10 did not apply before 2010]; CO2 threshold for millennial-scale oscillations in the climate system: implications for global warming scenarios (2007) [TEOS-10 did not apply before 2010]; Negative emissions—Part 1: Research landscape and synthesis (2018) [TEOS-10 does not appear]; FROT: A Framework to comprehensively describe radiative contributions to temperature responses (2024) [TEOS-10 does not appear]; Upwelling in the Southern Ocean (2015) [TEOS-10 does not appear]; Ekman-driven salt transport as a key mechanism for open-ocean polynya formation at Maud Rise (2024) [TEOS-10 does not appear]; Southern Ocean Deep Circulation and Heat Uptake in a High-Resolution Climate Model (2016 ) [TEOS-10 does not appear]; The Influence of Air-Sea CO2 Disequilibrium on Carbon Sequestration by the Ocean's Biological Pump (2024) [TEOS-10 does not appear]; Observing Antarctic Bottom Water in the Southern Ocean (2023) [TEOS-10 does not appear]; What Causes Anthropogenic Ocean Warming to Emerge from Internal Variability in a Coupled Model? (2022) [TEOS-10 was referenced]; Southern Ocean convection amplified past Antarctic warming and atmospheric CO2 rise during Heinrich Stadial 4 (2020) [TEOS-10 does not appear]; Rapid subsurface warming and circulation changes of Antarctic coastal waters by poleward shifting winds (2014) [TEOS-10 does not appear]; Physical controls of Southern Ocean deep-convection variability in CMIP5 models and the Kiel Climate Model (2017) [TEOS-10 does not appear]; Ocean carbon uptake under aggressive emission mitigation (2021) [TEOS-10 does not appear]; The global influence of localized dynamics in the Southern Ocean (2018) [no search made, not open access]; Reemergence of Anthropogenic Carbon Into the Ocean's Mixed Layer Strongly Amplifies Transient Climate Sensitivity (2020) [TEOS-10 does not appear]; A new scenario logic for the Paris Agreement long-term temperature goal (2019) [TEOS-10 does not appear]; The Effects of Ocean Heat Uptake on Transient Climate Sensitivity (2016) [TEOS-10 does not appear]; The Southern Hemisphere Westerlies in a Warming World: Propping Open the Door to the Deep Ocean (2006) [TEOS-10 did not apply before 2010]; The Oceanic Sink for Anthropogenic CO2 (2004) [TEOS-10 did not apply before 2010]; Localized subduction of anthropogenic carbon dioxide in the Southern Hemisphere oceans (2012) [TEOS-10 does not appear]; Sinks for Anthropogenic Carbon (2002) [TEOS-10 did not apply before 2010]; Processes and impacts of Arctic amplification: A research synthesis (2011) [TEOS-10 does not appear]; Southern Ocean Control of 2°C Global Warming in Climate Models (2022) [TEOS-10 does not appear]; The Effects of Ocean Heat Uptake on Transient Climate Sensitivity (2016) [TEOS-10 does not appear]; Observing Antarctic Bottom Water in the Southern Ocean (2023) [TEOS-10 does not appear]; Southern Ocean convection amplified past Antarctic warming and atmospheric CO2 rise during Heinrich Stadial 4 (2020) [TEOS-10 does not appear]; Rapid subsurface warming and circulation changes of Antarctic coastal waters by poleward shifting winds (2014) [TEOS-10 does not appear]; Acceleration of the ocean warming from 1961 to 2022 unveiled by large-ensemble reanalyses (2024) [TEOS-10 does not appear]; Closure of the Global Overturning Circulation Through the Indian, Pacific, and Southern Oceans: Schematics and Transports (2013) [TEOS-10 does not appear]; Spiraling pathways of global deep waters to the surface of the Southern Ocean (2017) [TEOS-10 does not appear]; Residence Time and Transformation of Warm Circumpolar Deep Water on the Antarctic Continental Shelf (2021) [TEOS-10 does not appear]; Path Independence of Carbon Budgets When Meeting a Stringent Global Mean Temperature Target After an Overshoot (2019) [TEOS-10 does not appear]; Path Independence of Carbon Budgets When Meeting a Stringent Global Mean Temperature Target After an Overshoot (2019) [TEOS-10 does not appear]; Ocean Carbon Pumps: Analysis of Relative Strengths and Efficiencies in Ocean-Driven Atmospheric CO2 Changes (1985) [TEOS-10 did not apply before 2010]; Heat stored in the Earth system: where does the energy go? (2020) [TEOS-10 does not appear]; An imperative to monitor Earth's energy imbalance (2016) [TEOS-10 does not appear]; The UVic earth system climate model: Model description, climatology, and applications to past, present and future climates (2010) [TEOS-10 does not appear]; Geochemical studies of the Weddell sea (1979) [TEOS-10 did not apply before 2010]; The role of the Southern Ocean in the global climate response to carbon emissions (2023) [TEOS-10 does not appear]; Regional Asymmetries in Ocean Heat and Carbon Storage due to Dynamic Redistribution in Climate Model Projections (2021) [TEOS-10 does not appear]; Asymmetries in the Southern Ocean contribution to global heat and carbon uptake (2024) [TEOS-10 does not appear]; The biological carbon pump in CMIP6 models: 21st century trends and uncertainties (2022) [TEOS-10 does not appear]; Connecting Changing Ocean Circulation with Changing Climate (2013) [TEOS-10 does not appear]; Importance of Ocean Heat Uptake Efficacy to Transient Climate Change (2010) [TEOS-10 does not appear]; Natural variability of Southern Ocean convection as a driver of observed climate trends (2018) [not searched, not open access]; Early Winter Triggering of the Maud Rise Polynya (2022) [TEOS-10 does not appear]; Sea Ice Production in the 2016 and 2017 Maud Rise Polynyas (2023) [TEOS-10 was referenced]; Is the climate response to CO2 emissions path dependent? (2012) [TEOS-10 does not appear]; Asymmetry in the climate–carbon cycle response to positive and negative CO2 emissions (2021) [TEOS-10 does not appear]; On the proportionality between global temperature change and cumulative CO2 emissions during periods of net negative CO2 emissions (2016) [TEOS-10 does not appear]; Net-zero approaches must consider Earth system impacts to achieve climate goals (2023) [TEOS-10 does not appear]; Observing the full ocean volume using Deep Argo floats (2023) [TEOS-10 does not appear];.
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