Greenhouse-gas forced changes in the Atlantic meridional overturning circulation and related worldwide sea-level change
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J. Gregory | W. Hurlin | Tatsuo Suzuki | J. Jungclaus | H. Haak | A. Hu | A. Köhl | O. Saenko | L. Zanna | Zipeng Yu | O. Garuba | A. Savita | M. Couldrey | Jiangbo Jin | Xiao Dong | Hailong Liu | S. Ojha
[1] Minghua Zhang,et al. Ocean Response to a Climate Change Heat-Flux Perturbation in an Ocean Model and Its Corresponding Coupled Model , 2022, Advances in Atmospheric Sciences.
[2] J. Jungclaus,et al. Response of northern North Atlantic and Atlantic meridional overturning circulation to reduced and enhanced wind stress forcing , 2021, Journal of Geophysical Research: Oceans.
[3] C. Domingues,et al. Super Residual Circulation: a new perspective on ocean vertical heat transport , 2021, Journal of Physical Oceanography.
[4] J. Marotzke,et al. Overturning Response to a Surface Wind Stress Doubling in an Eddying and a Non-Eddying Ocean , 2021, Journal of Physical Oceanography.
[5] J. Gregory,et al. Projecting Global Mean Sea‐Level Change Using CMIP6 Models , 2021, Geophysical Research Letters.
[6] Minghua Zhang,et al. CAS-ESM2.0 Model Datasets for the CMIP6 Flux-Anomaly-Forced Model Intercomparison Project (FAFMIP) , 2021, Advances in Atmospheric Sciences.
[7] J. Gregory,et al. Contribution of Ocean Physics and Dynamics at Different Scales to Heat Uptake in Low-Resolution AOGCMs , 2020, Journal of Climate.
[8] Xiaohong Liu,et al. Description and Climate Simulation Performance of CAS‐ESM Version 2 , 2020, Journal of Advances in Modeling Earth Systems.
[9] L. Talley,et al. Effects of Buoyancy and Wind Forcing on Southern Ocean Climate Change , 2020, Journal of Climate.
[10] Tatsuo Suzuki,et al. Future dynamic sea level change in the western subtropical North Pacific associated with ocean heat uptake and heat redistribution by ocean circulation under global warming , 2020, Progress in Earth and Planetary Science.
[11] C. Domingues,et al. Ocean Heat Storage in Response to Changing Ocean Circulation Processes , 2020, Journal of Climate.
[12] J. Gregory,et al. What causes the spread of model projections of ocean dynamic sea-level change in response to greenhouse gas forcing? , 2020, Climate Dynamics.
[13] M. Dix,et al. Configuration and spin-up of ACCESS-CM2, the new generation Australian Community Climate and Earth System Simulator Coupled Model , 2020, Journal of Southern Hemisphere Earth Systems Science.
[14] B. Fox‐Kemper,et al. Resolving and Parameterising the Ocean Mesoscale in Earth System Models , 2020, Current Climate Change Reports.
[15] P. Rasch,et al. A Partial Coupling Method to Isolate the Roles of the Atmosphere and Ocean in Coupled Climate Simulations , 2020, Journal of Advances in Modeling Earth Systems.
[16] Zhenghui Xie,et al. The Flexible Global Ocean‐Atmosphere‐Land System Model Grid‐Point Version 3 (FGOALS‐g3): Description and Evaluation , 2020, Journal of Advances in Modeling Earth Systems.
[17] Xuebin Zhang,et al. Regional Dynamic Sea Level Simulated in the CMIP5 and CMIP6 Models: Mean Biases, Future Projections, and Their Linkages , 2020, Journal of Climate.
[18] R. Wood,et al. Impact of ocean resolution and mean state on the rate of AMOC weakening , 2020, Climate Dynamics.
[19] Wei Cheng,et al. CMIP6 Models Predict Significant 21st Century Decline of the Atlantic Meridional Overturning Circulation , 2020, Geophysical Research Letters.
[20] J. Fyfe,et al. Ongoing AMOC and related sea-level and temperature changes after achieving the Paris targets , 2020, Nature Climate Change.
[21] C. Domingues,et al. ACCESS-OM2 v1.0: a global ocean–sea ice model at three resolutions , 2020, Geoscientific Model Development.
[22] W. G. Strand,et al. The Community Earth System Model Version 2 (CESM2) , 2020, Journal of Advances in Modeling Earth Systems.
[23] C. Domingues,et al. On the Superposition of Mean Advective and Eddy-Induced Transports in Global Ocean Heat and Salt Budgets , 2020, Journal of Climate.
[24] M. Jansen,et al. On freshwater fluxes and the Atlantic meridional overturning circulation , 2020, Limnology and Oceanography Letters.
[25] K. Taylor,et al. Causes of Higher Climate Sensitivity in CMIP6 Models , 2020, Geophysical Research Letters.
[26] J. Gregory,et al. Ocean‐Only FAFMIP: Understanding Regional Patterns of Ocean Heat Content and Dynamic Sea Level Change , 2020, Journal of Advances in Modeling Earth Systems.
[27] S. Xie,et al. Why Does Global Warming Weaken the Gulf Stream but Intensify the Kuroshio? , 2019, Journal of Climate.
[28] J. Jungclaus,et al. Max Planck Institute Earth System Model (MPI-ESM1.2) for the High-Resolution Model Intercomparison Project (HighResMIP) , 2018, Geoscientific Model Development.
[29] N. Gillett,et al. The Canadian Earth System Model version 5 (CanESM5.0.3) , 2019, Geoscientific Model Development.
[30] H. Tsujino,et al. The Meteorological Research Institute Earth System Model Version 2.0, MRI-ESM2.0: Description and Basic Evaluation of the Physical Component , 2019, Journal of the Meteorological Society of Japan. Ser. II.
[31] J. Seddon,et al. Description of the resolution hierarchy of the global coupled HadGEM3-GC3.1 model as used in CMIP6 HighResMIP experiments , 2019, Geoscientific Model Development.
[32] J. Gregory,et al. Concepts and Terminology for Sea Level: Mean, Variability and Change, Both Local and Global , 2019, Surveys in Geophysics.
[33] Alexander J. Winkler,et al. Developments in the MPI‐M Earth System Model version 1.2 (MPI‐ESM1.2) and Its Response to Increasing CO2 , 2019, Journal of advances in modeling earth systems.
[34] W. Liu,et al. Understanding the Uncertainty in the 21st Century Dynamic Sea Level Projections: The Role of the AMOC , 2019, Geophysical Research Letters.
[35] Antony Siahaan,et al. The Low‐Resolution Version of HadGEM3 GC3.1: Development and Evaluation for Global Climate , 2018, Journal of advances in modeling earth systems.
[36] Dai Yamazaki,et al. Description and basic evaluation of simulated mean state, internal variability, and climate sensitivity in MIROC6 , 2018, Geoscientific Model Development.
[37] Barry A. Klinger,et al. The Role of Individual Surface Flux Components in the Passive and Active Ocean Heat Uptake , 2018, Journal of Climate.
[38] J. Jungclaus,et al. Max Planck Institute Earth System Model (MPI-ESM1.2) for High-Resolution Model Intercomparison Project (HighResMIP) , 2018 .
[39] C. Heuzé. North Atlantic deep water formation and AMOC in CMIP5 models , 2017 .
[40] M. Huber,et al. Drivers of uncertainty in simulated ocean circulation and heat uptake , 2017 .
[41] L. Jackson,et al. The effect of model bias on Atlantic freshwater transport and implications for AMOC bi-stability , 2017 .
[42] O. Saenko,et al. Response of the North Atlantic dynamic sea level and circulation to Greenland meltwater and climate change in an eddy-permitting ocean model , 2017, Climate Dynamics.
[43] Jonathan M. Gregory,et al. The Flux-Anomaly-Forced Model Intercomparison Project (FAFMIP) contribution to CMIP6: investigation of sea-level and ocean climate change in response to CO 2 forcing , 2016 .
[44] Patrick Heimbach,et al. OMIP contribution to CMIP6: experimental and diagnostic protocol for the physical component of the Ocean Model Intercomparison Project , 2016 .
[45] The impact of SST biases on projections of anthropogenic climate change: A greater role for atmosphere‐only models? , 2016 .
[46] J. Sarmiento,et al. Mechanisms of Southern Ocean Heat Uptake and Transport in a Global Eddying Climate Model , 2016 .
[47] Veronika Eyring,et al. Overview of the Coupled Model Intercomparison Project Phase 6 (CMIP6) experimental design and organization , 2015 .
[48] C. Eden,et al. The Connection between Southern Ocean Winds, the Atlantic Meridional Overturning Circulation, and Indo-Pacific Upwelling , 2015 .
[49] Jonathan M. Gregory,et al. A process-based analysis of ocean heat uptake in an AOGCM with an eddy-permitting ocean component , 2015, Climate Dynamics.
[50] J. Gregory,et al. Ocean Heat Uptake Processes: A Model Intercomparison , 2015 .
[51] Jeffery R. Scott,et al. The ocean’s role in the transient response of climate to abrupt greenhouse gas forcing , 2015, Climate Dynamics.
[52] C. Wolfe,et al. Salt Feedback in the Adiabatic Overturning Circulation , 2014 .
[53] D. Stammer,et al. Projecting twenty-first century regional sea-level changes , 2014, Climatic Change.
[54] J. Gregory,et al. Attribution of the spatial pattern of CO2-forced sea level change to ocean surface flux changes , 2014 .
[55] William M. Putman,et al. Configuration and assessment of the GISS ModelE2 contributions to the CMIP5 archive , 2014 .
[56] Patrick Heimbach,et al. North Atlantic simulations in Coordinated Ocean-ice Reference Experiments phase II (CORE-II). Part I: Mean states , 2014 .
[57] B. Stevens,et al. Climate and carbon cycle changes from 1850 to 2100 in MPI‐ESM simulations for the Coupled Model Intercomparison Project phase 5 , 2013 .
[58] M. Meredith,et al. Remotely induced warming of Antarctic Bottom Water in the eastern Weddell gyre , 2013 .
[59] K. Kusahara,et al. Modeling Antarctic ice shelf responses to future climate changes and impacts on the ocean , 2013 .
[60] B. Samuels,et al. Connecting changing ocean circulation with changing climate , 2013 .
[61] Duo Yang,et al. Ocean Heat Transport and Its Projected Change in CanESM2 , 2012 .
[62] G. Vallis,et al. A Theory of the Interhemispheric Meridional Overturning Circulation and Associated Stratification , 2012 .
[63] Ronald,et al. GFDL’s ESM2 Global Coupled Climate–Carbon Earth System Models. Part I: Physical Formulation and Baseline Simulation Characteristics , 2012 .
[64] C. Jones,et al. The HadGEM2 family of Met Office Unified Model climate configurations , 2011 .
[65] Stephen M. Griffies,et al. Spatial Variability of Sea Level Rise in Twenty-First Century Projections , 2010 .
[66] R. Stouffer,et al. Model projections of rapid sea-level rise on the northeast coast of the United States , 2009 .
[67] T. Delworth,et al. Simulated impact of altered Southern Hemisphere winds on the Atlantic Meridional Overturning Circulation , 2008 .
[68] Stefan Rahmstorf,et al. On the driving processes of the Atlantic meridional overturning circulation , 2007 .
[69] J. Marotzke,et al. Regional Dynamic and Steric Sea Level Change in Response to the IPCC-A1B Scenario , 2007 .
[70] J. Gregory,et al. Understanding projections of sea level rise in a Hadley Centre coupled climate model , 2006 .
[71] B. Soden,et al. Robust Responses of the Hydrological Cycle to Global Warming , 2006 .
[72] Patrick Heimbach,et al. Estimating Eddy Stresses by Fitting Dynamics to Observations Using a Residual-Mean Ocean Circulation Model and Its Adjoint , 2005 .
[73] Mojib Latif,et al. The Max-Planck-Institute global ocean/sea ice model with orthogonal curvilinear coordinates , 2003 .
[74] John F. B. Mitchell,et al. The simulation of SST, sea ice extents and ocean heat transports in a version of the Hadley Centre coupled model without flux adjustments , 2000 .
[75] A. Gnanadesikan,et al. A simple predictive model for the structure of the oceanic pycnocline , 1999, Science.
[76] W. Munk,et al. Abyssal recipes II: energetics of tidal and wind mixing , 1998 .
[77] W. R. Holland,et al. Application of a Third-Order Upwind Scheme in the NCAR Ocean Model* , 1998 .
[78] Stephen M. Griffies,et al. The Gent–McWilliams Skew Flux , 1998 .
[79] 宇如聪. A Two-Step Shape-Preserving Advection Scheme , 1994 .
[80] P. Gent,et al. Isopycnal mixing in ocean circulation models , 1990 .
[81] P. Woodward,et al. The Piecewise Parabolic Method (PPM) for Gas Dynamical Simulations , 1984 .
[82] M. Cox. A primitive equation, 3-dimensional model of the ocean , 1984 .
[83] M. Redi. Oceanic Isopycnal Mixing by Coordinate Rotation , 1982 .