Greenhouse-gas forced changes in the Atlantic meridional overturning circulation and related worldwide sea-level change

[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 .