| 1 | A Synthesis of Global Coastal Ocean Greenhouse Gas Fluxes | 5.4 | 18 | Citations (PDF) |
| 2 | Enhanced CO2 uptake of the coastal ocean is dominated by biological carbon fixation | 18.3 | 46 | Citations (PDF) |
| 3 | A perspective on the next generation of Earth system model scenarios: towards representative emission pathways (REPs) | 3.8 | 26 | Citations (PDF) |
| 4 | ICON-Sapphire: simulating the components of the Earth system and their interactions at kilometer and subkilometer scales | 3.8 | 86 | Citations (PDF) |
| 5 | The representation of alkalinity and the carbonate pump from CMIP5 to CMIP6 Earth system models and implications for the carbon cycle | 3.1 | 23 | Citations (PDF) |
| 6 | Reconstructions and predictions of the global carbon budget with an emission-driven Earth system model | 5.9 | 11 | Citations (PDF) |
| 7 | Global Surface Ocean Acidification Indicators From 1750 to 2100 | 4.0 | 63 | Citations (PDF) |
| 8 | The Earth system model CLIMBER-X v1.0 – Part 2: The global carbon cycle | 3.8 | 14 | Citations (PDF) |
| 9 | Gross primary productivity and the predictability of CO<sub>2</sub>: more uncertainty in what we predict than how well we predict it | 3.1 | 9 | Citations (PDF) |
| 10 | Magnitude, Trends, and Variability of the Global Ocean Carbon Sink From 1985 to 2018 | 5.4 | 63 | Citations (PDF) |
| 11 | The New Max Planck Institute Grand Ensemble With CMIP6 Forcing and High‐Frequency Model Output | 4.0 | 39 | Citations (PDF) |
| 12 | Global Carbon Budget 2023 | 9.0 | 960 | Citations (PDF) |
| 13 | Transtorno de acumulação e perspectivas observadas no processo de envelhecer 2023, 15, | | 0 | Citations (PDF) |
| 14 | Oceanic Rossby waves drive inter-annual predictability of net primary production in the central tropical Pacific | 5.0 | 4 | Citations (PDF) |
| 15 | Local oceanic CO&lt;sub&gt;2&lt;/sub&gt; outgassing triggered by terrestrial carbon fluxes during deglacial flooding | 2.6 | 3 | Citations (PDF) |
| 16 | Increase in Arctic coastal erosion and its sensitivity to warming in the twenty-first century | 18.3 | 114 | Citations (PDF) |
| 17 | The ICON Earth System Model Version 1.0 | 4.0 | 50 | Citations (PDF) |
| 18 | Global Carbon Budget 2021 | 9.0 | 1,184 | Citations (PDF) |
| 19 | Ocean systems 2022, , 427-452 | | 2 | Citations (PDF) |
| 20 | Contrasting projections of the ENSO-driven CO<sub>2</sub>flux variability in the equatorial Pacific under high-warming scenario | 5.9 | 27 | Citations (PDF) |
| 21 | Seamless Integration of the Coastal Ocean in Global Marine Carbon Cycle Modeling | 4.0 | 37 | Citations (PDF) |
| 22 | Global Carbon Budget 2022 | 9.0 | 1,387 | Citations (PDF) |
| 23 | Improving scalability of Earth system models through coarse-grained component concurrency – a case study with the ICON v2.6.5 modelling system | 3.8 | 4 | Citations (PDF) |
| 24 | Ten new insights in climate science 2020 – a horizon scan | 4.3 | 19 | Citations (PDF) |
| 25 | Reconstructing the Preindustrial Coastal Carbon Cycle Through a Global Ocean Circulation Model: Was the Global Continental Shelf Already Both Autotrophic and a CO<sub>2</sub> Sink? | 5.4 | 35 | Citations (PDF) |
| 26 | Predictable Variations of the Carbon Sinks and Atmospheric CO<sub>2</sub>Growth in a Multi‐Model Framework | 4.2 | 23 | Citations (PDF) |
| 27 | Quantifying Errors in Observationally Based Estimates of Ocean Carbon Sink Variability | 5.4 | 99 | Citations (PDF) |
| 28 | The Climate Response to Emissions Reductions Due to COVID‐19: Initial Results From CovidMIP | 4.2 | 58 | Citations (PDF) |
| 29 | The Sensitivity of the Marine Carbonate System to Regional Ocean Alkalinity Enhancement | 3.9 | 58 | Citations (PDF) |
| 30 | Incorporating the stable carbon isotope &lt;sup&gt;13&lt;/sup&gt;C in the ocean biogeochemical component of the Max Planck Institute Earth System Model | 3.1 | 22 | Citations (PDF) |
| 31 | Historical increases in land‐derived nutrient inputs may alleviate effects of a changing physical climate on the oceanic carbon cycle | 11.1 | 43 | Citations (PDF) |
| 32 | A First Intercomparison of the Simulated LGM Carbon Results Within PMIP‐Carbon: Role of the Ocean Boundary Conditions | 2.9 | 14 | Citations (PDF) |
| 33 | Trivial improvements in predictive skill due to direct reconstruction of the global carbon cycle | 5.9 | 3 | Citations (PDF) |
| 34 | Opportunities and challenges in using remaining carbon budgets to guide climate policy | 11.9 | 111 | Citations (PDF) |
| 35 | Detectability of Artificial Ocean Alkalinization and Stratospheric Aerosol Injection in MPI‐ESM | 7.3 | 9 | Citations (PDF) |
| 36 | Time of Emergence and Large Ensemble Intercomparison for Ocean Biogeochemical Trends | 5.4 | 52 | Citations (PDF) |
| 37 | Tracking Improvement in Simulated Marine Biogeochemistry Between CMIP5 and CMIP6 | 7.8 | 233 | Citations (PDF) |
| 38 | Consistency and Challenges in the Ocean Carbon Sink Estimate for the Global Carbon Budget | 2.6 | 177 | Citations (PDF) |
| 39 | Microstructure and composition of marine aggregates as co-determinants for vertical particulate organic carbon transfer in the global ocean | 3.1 | 37 | Citations (PDF) |
| 40 | Oceanic CO&lt;sub&gt;2&lt;/sub&gt; outgassing and biological production hotspots induced by pre-industrial river loads of nutrients and carbon in a global modeling approach | 3.1 | 68 | Citations (PDF) |
| 41 | Twenty-first century ocean warming, acidification, deoxygenation, and upper-ocean nutrient and primary production decline from CMIP6 model projections | 3.1 | 580 | Citations (PDF) |
| 42 | Predictability Horizons in the Global Carbon Cycle Inferred From a Perfect‐Model Framework | 4.2 | 14 | Citations (PDF) |
| 43 | Inherent uncertainty disguises attribution of reduced atmospheric CO<sub>2</sub> growth to CO<sub>2</sub> emission reductions for up to a decade | 5.0 | 13 | Citations (PDF) |
| 44 | Carbon–concentration and carbon–climate feedbacks in CMIP6 models and their comparison to CMIP5 models | 3.1 | 405 | Citations (PDF) |
| 45 | Global Carbon Budget 2020 | 9.0 | 1,936 | Citations (PDF) |
| 46 | What was the source of the atmospheric CO&lt;sub&gt;2&lt;/sub&gt; increase during the Holocene? | 3.1 | 33 | Citations (PDF) |
| 47 | Thank You to Our 2018 Peer Reviewers | 4.2 | 0 | Citations (PDF) |
| 48 | Decadal trends in the ocean carbon sink | 7.5 | 124 | Citations (PDF) |
| 49 | The Max Planck Institute Grand Ensemble: Enabling the Exploration of Climate System Variability | 4.0 | 374 | Citations (PDF) |
| 50 | Predicting the variable ocean carbon sink | 11.5 | 38 | Citations (PDF) |
| 51 | Developments in the MPI‐M Earth System Model version 1.2 (MPI‐ESM1.2) and Its Response to Increasing CO<sub>2</sub> | 4.0 | 974 | Citations (PDF) |
| 52 | Carbonate Dissolution Enhanced by Ocean Stagnation and Respiration at the Onset of the Paleocene‐Eocene Thermal Maximum | 4.2 | 9 | Citations (PDF) |
| 53 | Detecting Regional Modes of Variability in Observation‐Based Surface Ocean <i>p</i>CO<sub>2</sub> | 4.2 | 45 | Citations (PDF) |
| 54 | The Zero Emissions Commitment Model Intercomparison Project (ZECMIP) contribution to C4MIP: quantifying committed climate changes following zero carbon emissions | 3.8 | 96 | Citations (PDF) |
| 55 | Global Carbon Budget 2019 | 9.0 | 1,351 | Citations (PDF) |
| 56 | Quantifying and Comparing Effects of Climate Engineering Methods on the Earth System | 7.3 | 22 | Citations (PDF) |
| 57 | Current and Future Decadal Trends in the Oceanic Carbon Uptake Are Dominated by Internal Variability | 4.2 | 48 | Citations (PDF) |
| 58 | Light absorption by marine cyanobacteria affects tropical climate mean state and variability | 5.9 | 9 | Citations (PDF) |
| 59 | Enhanced Rates of Regional Warming and Ocean Acidification After Termination of Large‐Scale Ocean Alkalinization | 4.2 | 17 | Citations (PDF) |
| 60 | Appreciation of 2017 GRL
Peer Reviewers | 4.2 | 0 | Citations (PDF) |
| 61 | The potential of &lt;sup&gt;230&lt;/sup&gt;Th for detection of ocean acidification impacts on pelagic carbonate production | 3.1 | 5 | Citations (PDF) |
| 62 | A Higher‐resolution Version of the Max Planck Institute Earth System Model (MPI‐ESM1.2‐HR) | 4.0 | 503 | Citations (PDF) |
| 63 | Global Carbon Budget 2018 | 9.0 | 1,386 | Citations (PDF) |
| 64 | Global Carbon Budget 2017 | 9.0 | 919 | Citations (PDF) |
| 65 | Rapid emergence of climate change in environmental drivers of marine ecosystems | 14.2 | 259 | Citations (PDF) |
| 66 | Towards real-time verification of CO2 emissions | 18.3 | 198 | Citations (PDF) |
| 67 | Incorporating a prognostic representation of marine nitrogen fixers into the global ocean biogeochemical model HAMOCC | 4.0 | 81 | Citations (PDF) |
| 68 | Amplification of global warming through pH dependence of DMS production simulated with a fully coupled Earth system model | 3.1 | 34 | Citations (PDF) |
| 69 | C4MIP – The Coupled Climate–Carbon Cycle Model Intercomparison Project:
experimental protocol for CMIP6 | 3.8 | 245 | Citations (PDF) |
| 70 | OMIP contribution to CMIP6: experimental and diagnostic protocol for the physical component of the Ocean Model Intercomparison Project | 3.8 | 284 | Citations (PDF) |
| 71 | Inconsistent strategies to spin up models in CMIP5: implications for ocean biogeochemical model performance assessment | 3.8 | 78 | Citations (PDF) |
| 72 | Net primary productivity estimates and environmental variables in the Arctic Ocean: An assessment of coupled physical-biogeochemical models | 3.0 | 41 | Citations (PDF) |
| 73 | Impacts of artificial ocean alkalinization on the carbon cycle and climate in Earth system simulations | 4.2 | 73 | Citations (PDF) |
| 74 | Appreciation of peer reviewers for 2015 | 4.2 | 0 | Citations (PDF) |
| 75 | Decadal predictions of the North Atlantic CO2 uptake | 14.2 | 48 | Citations (PDF) |
| 76 | Hidden trends in the ocean carbon sink | 34.3 | 6 | Citations (PDF) |
| 77 | New <em>Geophysical Research Letters</em> Editorial, Revisions Policies | 0.1 | 0 | Citations (PDF) |
| 78 | Evaluating the ocean biogeochemical components of Earth system models using atmospheric potential oxygen and ocean color data | 3.1 | 17 | Citations (PDF) |
| 79 | Corrigendum to "Evaluating the ocean biogeochemical components of Earth system models using atmospheric potential oxygen and ocean color data" published in Biogeosciences, 12, 193–208, 2015 | 3.1 | 0 | Citations (PDF) |
| 80 | Detection and Attribution of Climate Change Signal in Ocean Wind Waves | 4.5 | 44 | Citations (PDF) |
| 81 | The potential impact of ocean acidification upon eggs and larvae of yellowfin tuna ( Thunnus albacares ) | 2.4 | 51 | Citations (PDF) |
| 82 | Ocean biogeochemistry in the warm climate of the late Paleocene | 2.6 | 23 | Citations (PDF) |
| 83 | Global Carbon Budget 2015 | 9.0 | 663 | Citations (PDF) |
| 84 | Nonlinearity of Ocean Carbon Cycle Feedbacks in CMIP5 Earth System Models | 4.5 | 71 | Citations (PDF) |
| 85 | Global warming amplified by reduced sulphur fluxes as a result of ocean acidification | 18.3 | 122 | Citations (PDF) |
| 86 | Modelling the cycling of persistent organic pollutants (POPs) in the North Sea system: Fluxes, loading, seasonality, trends | 2.6 | 31 | Citations (PDF) |
| 87 | Anthropogenic perturbation of the carbon fluxes from land to ocean | 11.9 | 1,170 | Citations (PDF) |
| 88 | Carbon–Concentration and Carbon–Climate Feedbacks in CMIP5 Earth System Models | 4.5 | 615 | Citations (PDF) |
| 89 | Climate and carbon cycle changes from 1850 to 2100 in MPI‐ESM simulations for the Coupled Model Intercomparison Project phase 5 | 4.0 | 1,445 | Citations (PDF) |
| 90 | Global ocean biogeochemistry model HAMOCC: Model architecture and performance as component of the MPI‐Earth system model in different CMIP5 experimental realizations | 4.0 | 379 | Citations (PDF) |
| 91 | Assessing the potential of calcium-based artificial ocean alkalinization to mitigate rising atmospheric CO<sub>2</sub>and ocean acidification | 4.2 | 106 | Citations (PDF) |
| 92 | Future Arctic Ocean primary productivity from CMIP5 simulations: Uncertain outcome, but consistent mechanisms | 5.4 | 206 | Citations (PDF) |
| 93 | Impact of an extremely large magnitude volcanic eruption on the global climate and carbon cycle estimated from ensemble Earth System Model simulations | 3.1 | 24 | Citations (PDF) |
| 94 | Detecting an external influence on recent changes in oceanic oxygen using an optimal fingerprinting method | 3.1 | 37 | Citations (PDF) |
| 95 | Multiple stressors of ocean ecosystems in the 21st century: projections with CMIP5 models | 3.1 | 1,363 | Citations (PDF) |
| 96 | Detecting regional anthropogenic trends in ocean acidification against natural variability | 18.3 | 91 | Citations (PDF) |
| 97 | Detection and projection of carbonate dissolution in the water column and deep‐sea sediments due to ocean acidification | 4.2 | 34 | Citations (PDF) |
| 98 | Modelling the fate of persistent organic pollutants (POPs) in the North Sea system | 1.4 | 8 | Citations (PDF) |
| 99 | Scenarios of Temporal and Spatial Evolution of Hexabromocyclododecane in the North Sea | 11.3 | 6 | Citations (PDF) |
| 100 | Detecting early signs of global-scale effects of ocean acidification on marine calcification | 0.4 | 0 | Citations (PDF) |
| 101 | Changes in underwater sound propagation caused by ocean acidification | 0.4 | 3 | Citations (PDF) |
| 102 | Future ocean increasingly transparent to low-frequency sound owing to carbon dioxide emissions | 11.9 | 53 | Citations (PDF) |
| 103 | Changes in underwater sound propagation caused by ocean acidification | 0.4 | 2 | Citations (PDF) |
| 104 | Detecting early signs of global-scale effects of ocean acidification on marine calcification | 0.4 | 0 | Citations (PDF) |
| 105 | Mass budgets and contribution of individual sources and sinks to the abundance of γ-HCH, α-HCH and PCB 153 in the North Sea | 8.5 | 13 | Citations (PDF) |
| 106 | Bestimmung des Ferntransports von persistenten organischen Spurenstoffen und der Umweltexposition mittels Modelluntersuchungen | 0.3 | 3 | Citations (PDF) |
| 107 | A fate and transport ocean model for persistent organic pollutants and its application to the North Sea | 2.6 | 66 | Citations (PDF) |
