Partitioning climate projection uncertainty with multiple large ensembles and CMIP5/6

Abstract. Partitioning uncertainty in projections of future climate change into contributions from internal variability, model response uncertainty and emissions scenarios has historically relied on making assumptions about forced changes in the mean and variability. With the advent of multiple single-model initial-condition large ensembles (SMILEs), these assumptions can be scrutinized, as they allow a more robust separation between sources of uncertainty. Here, the framework from Hawkins and Sutton (2009) for uncertainty partitioning is revisited for temperature and precipitation projections using seven SMILEs and the Coupled Model Intercomparison Project CMIP5 and CMIP6 archives. The original approach is shown to work well at global scales (potential method bias < 20 %), while at local to regional scales such as British Isles temperature or Sahel precipitation, there is a notable potential method bias (up to 50 %), and more accurate partitioning of uncertainty is achieved through the use of SMILEs. Whenever internal variability and forced changes therein are important, the need to evaluate and improve the representation of variability in models is evident. The available SMILEs are shown to be a good representation of the CMIP5 model diversity in many situations, making them a useful tool for interpreting CMIP5. CMIP6 often shows larger absolute and relative model uncertainty than CMIP5, although part of this difference can be reconciled with the higher average transient climate response in CMIP6. This study demonstrates the added value of a collection of SMILEs for quantifying and diagnosing uncertainty in climate projections.

[1]  M. Long,et al.  Time of Emergence and Large Ensemble Intercomparison for Ocean Biogeochemical Trends , 2020, Global biogeochemical cycles.

[2]  J. Marotzke,et al.  Quantifying the role of internal variability in the temperature we expect to observe in the coming decades , 2020, Environmental Research Letters.

[3]  R. Knutti,et al.  Reduced global warming from CMIP6 projections when weighting models by performance and independence , 2020, Earth System Dynamics.

[4]  J. Randerson,et al.  Insights from Earth system model initial-condition large ensembles and future prospects , 2020, Nature Climate Change.

[5]  Christopher J. Smith,et al.  Past warming trend constrains future warming in CMIP6 models , 2020, Science Advances.

[6]  Lukas Gudmundsson,et al.  Emulating Earth system model temperatures with MESMER: from global mean temperature trajectories to grid-point-level realizations on land , 2018, Earth System Dynamics.

[7]  K. Taylor,et al.  Causes of Higher Climate Sensitivity in CMIP6 Models , 2020, Geophysical Research Letters.

[8]  B. Samset,et al.  How Daily Temperature and Precipitation Distributions Evolve With Global Surface Temperature. , 2019, Earth's Future.

[9]  N. Maher,et al.  How large does a large ensemble need to be? , 2019, Earth System Dynamics.

[10]  J. Hurrell,et al.  Viewing Forced Climate Patterns Through an AI Lens , 2019, Geophysical Research Letters.

[11]  E. Hawkins,et al.  Observed Emergence of the Climate Change Signal: From the Familiar to the Unknown , 2019, Geophysical Research Letters.

[12]  R. Knutti,et al.  Quantifying uncertainty in European climate projections using combined performance-independence weighting , 2019, Environmental Research Letters.

[13]  T. Mauritsen,et al.  Emergent constraints on Earth’s transient and equilibrium response to doubled CO2 from post-1970s global warming , 2019, Nature Geoscience.

[14]  R. Sutton Climate Science Needs to Take Risk Assessment Much More Seriously , 2019, Bulletin of the American Meteorological Society.

[15]  N. Meinshausen,et al.  Uncovering the Forced Climate Response from a Single Ensemble Member Using Statistical Learning , 2019, Journal of Climate.

[16]  J. Sarmiento,et al.  Emergence of Anthropogenic Signals in the Ocean Carbon Cycle , 2019, Nature Climate Change.

[17]  N. Gillett,et al.  The Canadian Earth System Model version 5 (CanESM5.0.3) , 2019, Geoscientific Model Development.

[18]  B. Stevens,et al.  The Max Planck Institute Grand Ensemble: Enabling the Exploration of Climate System Variability , 2019, Journal of Advances in Modeling Earth Systems.

[19]  Stephen A. Klein,et al.  Progressing emergent constraints on future climate change , 2019, Nature Climate Change.

[20]  A. Hall Progressing Emergent Constraints on Future Climate Change 1 2 , 2019 .

[21]  Jochem Marotzke,et al.  Quantifying the irreducible uncertainty in near‐term climate projections , 2018, WIREs Climate Change.

[22]  J. Marotzke,et al.  ENSO Change in Climate Projections: Forced Response or Internal Variability? , 2018, Geophysical Research Letters.

[23]  Elizabeth A. Barnes,et al.  Modeled and Observed Multidecadal Variability in the North Atlantic Jet Stream and Its Connection to Sea Surface Temperatures , 2018 .

[24]  Biased Estimates of Changes in Climate Extremes From Prescribed SST Simulations , 2018, Geophysical Research Letters.

[25]  C. Deser,et al.  Evolution of the Global Coupled Climate Response to Arctic Sea Ice Loss during 1990–2090 and Its Contribution to Climate Change , 2018, Journal of Climate.

[26]  C. Deser,et al.  Internal Variability and Regional Climate Trends in an Observational Large Ensemble , 2018, Journal of Climate.

[27]  Robert Pincus,et al.  ESD Reviews: Model dependence in multi-model climate ensembles: weighting, sub-selection and out-of-sample testing , 2018, Earth System Dynamics.

[28]  C. Deser,et al.  Attributing the U.S. Southwest's Recent Shift Into Drier Conditions , 2018, Geophysical Research Letters.

[29]  M. England,et al.  On the Choice of Ensemble Mean for Estimating the Forced Signal in the Presence of Internal Variability , 2018, Journal of Climate.

[30]  C. Deser,et al.  How Well Do We Know ENSO’s Climate Impacts over North America, and How Do We Evaluate Models Accordingly? , 2018, Journal of Climate.

[31]  E. Fischer,et al.  Prospects and Caveats of Weighting Climate Models for Summer Maximum Temperature Projections Over North America , 2018 .

[32]  E. Fischer,et al.  Influence of blocking on Northern European and Western Russian heatwaves in large climate model ensembles , 2018 .

[33]  J. Wallace,et al.  Disentangling Global Warming, Multidecadal Variability, and El Niño in Pacific Temperatures , 2018 .

[34]  W. G. Strand,et al.  Predicting Near-Term Changes in the Earth System: A Large Ensemble of Initialized Decadal Prediction Simulations Using the Community Earth System Model , 2018, Bulletin of the American Meteorological Society.

[35]  Auroop R. Ganguly,et al.  Intercomparison of model response and internal variability across climate model ensembles , 2018, Climate Dynamics.

[36]  C. Deser,et al.  Precipitation variability increases in a warmer climate , 2017, Scientific Reports.

[37]  E. Fischer,et al.  Potential to Constrain Projections of Hot Temperature Extremes , 2017 .

[38]  Young‐Oh Kwon,et al.  Estimation of the SST Response to Anthropogenic and External Forcing and Its Impact on the Atlantic Multidecadal Oscillation and the Pacific Decadal Oscillation , 2017 .

[39]  Spencer A. Hill,et al.  Change in the magnitude and mechanisms of global temperature variability with warming , 2017, Nature climate change.

[40]  C. Deser,et al.  Toward a New Estimate of “Time of Emergence” of Anthropogenic Warming: Insights from Dynamical Adjustment and a Large Initial-Condition Model Ensemble , 2017 .

[41]  Karen A. McKinnon,et al.  An “Observational Large Ensemble” to Compare Observed and Modeled Temperature Trend Uncertainty due to Internal Variability , 2017 .

[42]  J. Smerdon,et al.  Projected drought risk in 1.5°C and 2°C warmer climates , 2017 .

[43]  Ruth Lorenz,et al.  A climate model projection weighting scheme accounting for performance and interdependence , 2017 .

[44]  John F. B. Mitchell,et al.  THE WCRP CMIP 3 MULTIMODEL DATASET A New Era in Climate Change Research , 2017 .

[45]  F. Zwiers,et al.  Attribution of Extreme Events in Arctic Sea Ice Extent , 2017 .

[46]  J. Eom,et al.  The Shared Socioeconomic Pathways and their energy, land use, and greenhouse gas emissions implications: An overview , 2017 .

[47]  Brian C. O'Neill,et al.  The Scenario Model Intercomparison Project (ScenarioMIP) for CMIP6 , 2016 .

[48]  S. Coats,et al.  The challenge of accurately quantifying future megadrought risk in the American Southwest , 2016, Geophysical research letters.

[49]  K. Lindsay,et al.  Partitioning uncertainty in ocean carbon uptake projections: Internal variability, emission scenario, and model structure , 2016 .

[50]  W. Cheung,et al.  Sources of uncertainties in 21st century projections of potential ocean ecosystem stressors , 2016 .

[51]  G. Hegerl,et al.  The importance of ENSO phase during volcanic eruptions for detection and attribution , 2016 .

[52]  Ed Hawkins,et al.  Robust Future Changes in Temperature Variability under Greenhouse Gas Forcing and the Relationship with Thermal Advection , 2016 .

[53]  C. Deser,et al.  Forced and Internal Components of Winter Air Temperature Trends over North America during the past 50 Years: Mechanisms and Implications* , 2016 .

[54]  F. Joos,et al.  Transient Earth system responses to cumulative carbon dioxide emissions: linearities, uncertainties, and probabilities in an observation-constrained model ensemble , 2016 .

[55]  W. G. Strand,et al.  A new ensemble of GCM simulations to assess avoided impacts in a climate mitigation scenario , 2018, Climatic Change.

[56]  J. Gregory,et al.  Irreducible uncertainty in near-term climate projections , 2016, Climate Dynamics.

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

[58]  K.,et al.  The Community Earth System Model (CESM) large ensemble project: a community resource for studying climate change in the presence of internal climate variability , 2015 .

[59]  O. Boucher,et al.  Why Does Aerosol Forcing Control Historical Global-Mean Surface Temperature Change in CMIP5 Models? , 2015 .

[60]  Reto Knutti,et al.  A Representative Democracy to Reduce Interdependency in a Multimodel Ensemble , 2015 .

[61]  Reto Knutti,et al.  Addressing interdependency in a multimodel ensemble by interpolation of model properties , 2015 .

[62]  J. Wallace,et al.  Dynamical Adjustment of the Northern Hemisphere Surface Air Temperature Field: Methodology and Application to Observations* , 2015 .

[63]  John P. Krasting,et al.  Dominance of the Southern Ocean in Anthropogenic Carbon and Heat Uptake in CMIP5 Models , 2015 .

[64]  E. Guilyardi,et al.  Bidecadal North Atlantic ocean circulation variability controlled by timing of volcanic eruptions , 2014, Nature Communications.

[65]  N. Diffenbaugh,et al.  Influence of temperature and precipitation variability on near-term snow trends , 2015, Climate Dynamics.

[66]  Keith B. Rodgers,et al.  Emergence of multiple ocean ecosystem drivers in a large ensemble suite with an Earth system model , 2014 .

[67]  E. Fischer,et al.  Models agree on forced response pattern of precipitation and temperature extremes , 2014 .

[68]  J. Screen,et al.  Arctic amplification decreases temperature variance in northern mid- to high-latitudes , 2014 .

[69]  R. Knutti,et al.  Robustness and uncertainties in the new CMIP5 climate model projections , 2013 .

[70]  Reto Knutti,et al.  Climate model genealogy: Generation CMIP5 and how we got there , 2013 .

[71]  S. Jeffrey,et al.  Australia's CMIP5 submission using the CSIRO-Mk3.6 model , 2013 .

[72]  T. Andrews,et al.  Evaluating adjusted forcing and model spread for historical and future scenarios in the CMIP5 generation of climate models , 2013 .

[73]  L. Brekke,et al.  Uncertainties in Projections of Future Changes in Extremes , 2013 .

[74]  Stephen Jeffrey,et al.  Australia ’ s CMIP 5 submission using the CSIRO-Mk 3 . 6 model , 2013 .

[75]  J. Curry,et al.  Berkeley Earth Temperature Averaging Process , 2013 .

[76]  E. Fischer,et al.  Changes in European summer temperature variability revisited , 2012 .

[77]  J. Wallace,et al.  Simulated versus observed patterns of warming over the extratropical Northern Hemisphere continents during the cold season , 2012, Proceedings of the National Academy of Sciences.

[78]  A. Ganguly,et al.  Evaluation of global climate models for Indian monsoon climatology , 2012 .

[79]  D. Rowell Sources of uncertainty in future changes in local precipitation , 2012, Climate Dynamics.

[80]  E. Hawkins,et al.  A Simple, Coherent Framework for Partitioning Uncertainty in Climate Predictions , 2011 .

[81]  Reto Knutti,et al.  Early onset of significant local warming in low latitude countries , 2011 .

[82]  E. Hawkins,et al.  The potential to narrow uncertainty in projections of regional precipitation change , 2011 .

[83]  R. Knutti,et al.  Spatial-Scale Dependence of Climate Model Performance in the CMIP3 Ensemble , 2011 .

[84]  C. Deser,et al.  Uncertainty in climate change projections: the role of internal variability , 2012, Climate Dynamics.

[85]  A. Sterl,et al.  EC-Earth A Seamless earth-System Prediction Approach in Action , 2010 .

[86]  Veronika Eyring,et al.  A Summary of the CMIP5 Experiment Design , 2010 .

[87]  P. O'Gorman,et al.  The physical basis for increases in precipitation extremes in simulations of 21st-century climate change , 2009, Proceedings of the National Academy of Sciences.

[88]  E. Hawkins,et al.  The Potential to Narrow Uncertainty in Regional Climate Predictions , 2009 .

[89]  Richard L. Smith,et al.  Bayesian Modeling of Uncertainty in Ensembles of Climate Models , 2009 .

[90]  D. Stone,et al.  Towards constraining climate sensitivity by linear analysis of feedback patterns in thousands of perturbed-physics GCM simulations , 2008 .

[91]  G. Roe,et al.  Why Is Climate Sensitivity So Unpredictable? , 2007, Science.

[92]  John F. B. Mitchell,et al.  THE WCRP CMIP3 Multimodel Dataset: A New Era in Climate Change Research , 2007 .

[93]  Reto Knutti,et al.  The use of the multi-model ensemble in probabilistic climate projections , 2007, Philosophical Transactions of the Royal Society A: Mathematical, Physical and Engineering Sciences.

[94]  D A Stainforth,et al.  Confidence, uncertainty and decision-support relevance in climate predictions , 2007, Philosophical Transactions of the Royal Society A: Mathematical, Physical and Engineering Sciences.

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

[96]  G. Branstator,et al.  Tropical origins for recent and future Northern Hemisphere climate change , 2004 .

[97]  M. Webb,et al.  Quantification of modelling uncertainties in a large ensemble of climate change simulations , 2004, Nature.

[98]  J. Janowiak,et al.  The Version 2 Global Precipitation Climatology Project (GPCP) Monthly Precipitation Analysis (1979-Present) , 2003 .

[99]  F. Giorgi,et al.  Calculation of average, uncertainty range, and reliability of regional climate changes from AOGCM simulations via the reliability ensemble averaging (REA) method , 2002 .

[100]  M. R. Allen,et al.  Checking for model consistency in optimal fingerprinting , 1999 .

[101]  Linda O. Mearns,et al.  MEAN AND VARIANCE CHANGE IN CLIMATE SCENARIOS: METHODS, AGRICULTURAL APPLICATIONS, AND MEASURES OF UNCERTAINTY , 1997 .

[102]  K. Hasselmann On the signal-to-noise problem in atmospheric response studies , 1979 .

[103]  E. Lorenz Deterministic nonperiodic flow , 1963 .