Consistency of the regional response to global warming levels from CMIP5 and CORDEX projections

[1]  Dr. Kirstin K. Holsman.  Climate Change 2022 – Impacts, Adaptation and Vulnerability , 2023 .

[2]  S. Somot,et al.  Mechanisms behind large-scale inconsistencies between regional and global climate model-based projections over Europe , 2022, Climate Dynamics.

[3]  José M. Gutiérrez,et al.  The worldwide C3S CORDEX grand ensemble: A major contribution to assess regional climate change in the IPCC AR6 Atlas , 2022, Bulletin of the American Meteorological Society.

[4]  A. Casanueva,et al.  Implementation of FAIR principles in the IPCC: the WGI AR6 Atlas repository , 2022, Scientific Data.

[5]  L. Polvani,et al.  Arctic amplification, and its seasonal migration, over a wide range of abrupt CO2 forcing , 2022, npj Climate and Atmospheric Science.

[6]  Zuo Zhi-Yan,et al.  Linking global to regional climate change , 2021 .

[7]  F. Giorgi,et al.  The CORDEX-CORE EXP-I initiative: Description and highlight results from the initial analysis , 2021, Bulletin of the American Meteorological Society.

[8]  Antonio S. Cofiño,et al.  Repository supporting the implementation of FAIR principles in the IPCC-WGI Atlas , 2021 .

[9]  R. Schiemann,et al.  Land–Atmosphere Coupling Sensitivity to GCMs Resolution: A Multimodel Assessment of Local and Remote Processes in the Sahel Hot Spot , 2020, Journal of Climate.

[10]  S. Seneviratne,et al.  Regional Climate Sensitivity of Climate Extremes in CMIP6 Versus CMIP5 Multimodel Ensembles , 2020, Earth's future.

[11]  W. J. Gutowski,et al.  The Ongoing Need for High-Resolution Regional Climate Models: Process Understanding and Stakeholder Information , 2020, Bulletin of the American Meteorological Society.

[12]  Richard G. Jones,et al.  Regional climate downscaling over Europe: perspectives from the EURO-CORDEX community , 2020, Regional Environmental Change.

[13]  Kevin Hennessy,et al.  An update of IPCC climate reference regions for subcontinental analysis of climate model data: definition and aggregated datasets , 2020, Earth System Science Data.

[14]  F. Giorgi,et al.  A new spatially distributed added value index for regional climate models: the EURO-CORDEX and the CORDEX-CORE highest resolution ensembles , 2020, Climate Dynamics.

[15]  F. Giorgi,et al.  Assessing mean climate change signals in the global CORDEX-CORE ensemble , 2020, Climate Dynamics.

[16]  S. Somot,et al.  Large discrepancies in summer climate change over Europe as projected by global and regional climate models: causes and consequences , 2020, Climate Dynamics.

[17]  Richard Wartenburger,et al.  Regional climate model projections underestimate future warming due to missing plant physiological CO2 response , 2019, Environmental Research Letters.

[18]  B. Hewitson,et al.  What can we know about future precipitation in Africa? Robustness, significance and added value of projections from a large ensemble of regional climate models , 2019, Climate Dynamics.

[19]  R. Vautard,et al.  The benefits of increasing resolution in global and regional climate simulations for European climate extremes , 2019, Geoscientific Model Development.

[20]  S. Seneviratne,et al.  Importance of Framing for Extreme Event Attribution: The Role of Spatial and Temporal Scales , 2019, Earth's Future.

[21]  J. Christensen,et al.  Robustness and Scalability of Regional Climate Projections Over Europe , 2019, Front. Environ. Sci..

[22]  Laurent Z. X. Li,et al.  Assessment of CORDEX simulations over South America: added value on seasonal climatology and resolution considerations , 2018, Climate Dynamics.

[23]  S. Somot,et al.  The effects of 1.5 and 2 degrees of global warming on Africa in the CORDEX ensemble , 2018, Environmental Research Letters.

[24]  A. Bodas‐Salcedo,et al.  Quantifying climate feedbacks in polar regions , 2018, Nature Communications.

[25]  S. Seneviratne,et al.  Changes in regional climate extremes as a function of global mean temperature: an interactive plotting framework , 2017 .

[26]  M. Déqué,et al.  A multi-model climate response over tropical Africa at +2°C , 2017 .

[27]  O. B. Christensen,et al.  The effect of the pathway to a two degrees warmer world on the regional temperature change of Europe , 2017 .

[28]  Michel Rixen,et al.  WCRP COordinated Regional Downscaling EXperiment (CORDEX): A diagnostic MIP for CMIP6 , 2016 .

[29]  Erika Coppola,et al.  Enhanced summer convective rainfall at Alpine high elevations in response to climate warming , 2016 .

[30]  S. Seneviratne,et al.  Allowable CO2 emissions based on regional and impact-related climate targets , 2016, Nature.

[31]  Veronika Eyring,et al.  Overview of the Coupled Model Intercomparison Project Phase 6 (CMIP6) experimental design and organization , 2015 .

[32]  F. Giorgi,et al.  Regional Dynamical Downscaling and the Cordex Initiative , 2015 .

[33]  B. Sanderson,et al.  Does extreme precipitation intensity depend on the emissions scenario? , 2015 .

[34]  Dhruva R. Chakrabarti,et al.  Atlas , 2014, OOPSLA.

[35]  Karl E. Taylor,et al.  An overview of CMIP5 and the experiment design , 2012 .

[36]  Toru Nozawa,et al.  Temperature scaling pattern dependence on representative concentration pathway emission scenarios , 2012, Climatic Change.

[37]  C. Bretherton,et al.  The Soil Moisture–Precipitation Feedback in Simulations with Explicit and Parameterized Convection , 2009 .

[38]  S. Seneviratne,et al.  Land–atmosphere coupling and climate change in Europe , 2006, Nature.

[39]  J. Overpeck,et al.  Climate Change 2007: The Physical Science Basis , 2007 .

[40]  T. Wilbanks,et al.  Contribution of Working Group II to the Fourth Assessment Report of the Intergovernmental Panel on Climate Change , 2007 .