Climate model genealogy: Generation CMIP5 and how we got there
Open accessAbstract
A new ensemble of climate models is becoming available and provides the basis for climate change projections. Here, we show a first analysis indicating that the models in the new ensemble agree better with observations than those in older ones and that the poorest models have been eliminated. Most models are strongly tied to their predecessors, and some also exchange ideas and code with other models, thus supporting an earlier hypothesis that the models in the new ensemble are neither independent of each other nor independent of the earlier generation. On the basis of one atmosphere model, we show how statistical methods can identify similarities between model versions and complement process understanding in characterizing how and why a model has changed. We argue that the interdependence of models complicates the interpretation of multimodel ensembles but largely goes unnoticed.
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- Findingnone given
Some CMIP5 models exchange ideas and code with other models.
“and some also exchange ideas and code with other models”
Quote in the paperSubstantial claim - Findingown data
The CMIP5 models agree better with observations than the older CMIP2 and CMIP3 models.
“Here, we show a first analysis indicating that the models in the new ensemble agree better with observations than those in older ones”
- Also stated in: § 2. Results · plain
“CMIP5 continues the trend of better agreement with observations [Reichler and Kim, 2008], with the mean distance from observations reduced by approximately 20% from CMIP3 to CMIP5.”
Quote in the paperSubstantial claim0 of 1 sources checked- cites Reichler and Kim, 2008
Not checked in the free run.
- Also stated in: § 2. Results · plain
- Findingnone given
Most CMIP5 models are strongly tied to their predecessors.
“Most models are strongly tied to their predecessors”
Quote in the paperSubstantial claim - Findingown data
Statistical methods can identify similarities between model versions and complement process understanding in characterizing how and why a model has changed.
“On the basis of one atmosphere model, we show how statistical methods can identify similarities between model versions and complement process understanding in characterizing how and why a model has changed.”
Quote in the paperSubstantial claim - Findingnone given
The distance between models from the same institutions is often a factor of three to ten smaller than the distance to other models.
“The distance between models from the same institutions is often a factor of three to ten smaller than that to other models.”
Quote in the paperSubstantial claim
- Findingnone given
Sharing of model code became more widespread in CMIP5 than in CMIP3.
“Sharing of model code occurred in CMIP3 (e.g., the Italian INGV model using an ECHAM atmosphere, or the Norwegian BCCR using the French ARPEGE atmosphere also present in CNRM) but has become more widespread in CMIP5.”
Quote in the paperNot a substantial claim - Findingreasoning
The strengths and weaknesses of particular models are partly passed on to newer model versions and to other models by the exchange of code and ideas.
“The strengths and weaknesses of particular models, as they are evident in the biases in simulating present day climate, are partly passed on to newer model versions and to other models by the exchange of code and ideas.”
Quote in the paperSubstantial claim - Findingown data
The contribution of internal unforced variability is small for this metric.
“The contribution of internal unforced variability (quantified using multiple segments of a control simulation) is small for this metric”
Quote in the paperNot a substantial claim - Findingnone given
The CAM models with the most similar physics packages cluster closest together.
“In general, the CAM models with the most similar physics packages cluster closest together.”
Quote in the paperSubstantial claim - Findingreasoning
The similarity metric is strongly determined by biases in present-day climatology and seasonal cycle, that is, by model differences rather than initial conditions or forcing.
“The similarity metric is defined from the unperturbed preindustrial model control state and is strongly determined by biases in the present day climatology and seasonal cycle, that is, by model differences rather than initial conditions or forcing.”
Quote in the paperSubstantial claim - Findingcitation
The mean distance from observations for CMIP5 is reduced by approximately 20% from CMIP3 to CMIP5.
“CMIP5 continues the trend of better agreement with observations [Reichler and Kim, 2008], with the mean distance from observations reduced by approximately 20% from CMIP3 to CMIP5.”
Quote in the paperNot a substantial claim0 of 1 sources checked- cites Reichler and Kim, 2008
Not checked in the free run.
- Premisecitation
Models from different centers that share the same atmospheric model, even in different versions, are closely related.
“models in different centers sharing the same atmospheric model (even in different versions) were also closely related”
Quote in the paperSubstantial claim0 of 1 sources checked- cites Masson and Knutti, 2011
Not checked in the free run.
- Interpretationreasoning
The interdependence of models complicates the interpretation of multimodel ensembles.
“We argue that the interdependence of models complicates the interpretation of multimodel ensembles but largely goes unnoticed.”
Quote in the paperSubstantial claim - Premisecitation
Models from the same centers are often very similar in their present-day climatology.
“Models from the same centers were shown in MK11 to often be very similar in their present day climatology”
Quote in the paperSubstantial claim0 of 1 sources checked- cites Masson and Knutti, 2011
Not checked in the free run.
- Interpretationreasoning
The new generation of global climate models in CMIP5 supports the idea of a rather gradual evolutionary process by which models improve over time.
“The new generation of global climate models in CMIP5 supports the idea of a rather gradual evolutionary process by which models improve over time.”
Quote in the paperSubstantial claim - Premisecitation
The biggest change in climate sensitivity from CAM4 to CAM5 results from the change to the shallow convection scheme, which increases shortwave cloud feedbacks.
“As discussed by Gettelman et al. [2012], the biggest change in climate sensitivity results from the change to the shallow convection scheme, which increases shortwave cloud feedbacks.”
Quote in the paperNot a substantial claim0 of 1 sources checked- cites Gettelman et al., 2012
Not checked in the free run.
- Interpretationreasoning
Observational uncertainties may explain some of the remaining model biases.
“observational uncertainties (estimated from differences across multiple data sets) may explain some of the remaining model biases”
Quote in the paperNot a substantial claim - Interpretationreasoning
The fact that the ensemble compares more favorably with observations despite enhanced complexity is perhaps one indication that the development strategy of adding complexity is successful in better representing the current climate system.
“However, the fact that the ensemble compares more favorably with observations, despite the enhanced complexity of many of the models, is perhaps one indication that this development strategy of using enhancements in computational power to add complexity is successful in better representing the current climate system.”
Quote in the paperSubstantial claim - Interpretationreasoning
Shared code and data sets reduce the effective degrees of freedom in a multimodel ensemble.
“Shared code and data sets reduce the effective degrees of freedom in a multimodel ensemble.”
Quote in the paperSubstantial claim - Interpretationcitation
Projected climate change is often not related to the climatological mean bias in an obvious way.
“This is consistent with the fact that the projected climate change is often not related to the climatological mean bias in an obvious way, a difficulty seen in many studies [Knutti et al., 2010].”
Quote in the paperNot a substantial claim0 of 1 sources checked- cites Knutti et al., 2010
Not checked in the free run.
- Premisenone given
In most studies, all models are treated equally, giving more weight to centers that submitted multiple versions or shared their code with others.
“In most studies (including in the IPCC reports), all models are treated equally, thus giving more weight to those who have submitted multiple versions or share their code with others.”
Quote in the paperSubstantial claim
- May combine two claims. 10
- The quote only partly states this claim. 1
- Classified as probably not a substantial claim. 7
May combine two claims. The quote only partly states this claim.
Findingnone givenThe poorest models in the CMIP ensemble have been eliminated or have improved the most.
“and that the poorest models have been eliminated”
Quote in the paperSubstantial claimMay combine two claims.
Findingown dataThe CAM5 experiments cluster together, with three single perturbation experiments similar to the base CAM5 experiment.
“As is clear from the tree shown in Figure 2a, the CAM5 experiments cluster together, with three single perturbation experiments similar to the base CAM5 experiment.”
Quote in the paperNot a substantial claimMay combine two claims.
FindingcitationDifferent observation and reanalysis data sets cluster together, and the rankings are nearly identical irrespective of the chosen data set.
“as shown already by MK11, the different observation and reanalysis data set cluster together (see Figure 1a), and the rankings in Figure 3 are nearly identical irrespective of the chosen data set.”
Quote in the paperNot a substantial claim0 of 1 sources checked- cites Masson and Knutti, 2011
Not checked in the free run.
May combine two claims.
FindingreasoningFor projected changes, some models remain close, while other similarities do not persist.
“For the projected changes, some models remain close (e.g., those which share a similar atmosphere), whereas other similarities do not persist (e.g., if the new version of a model has a different climate sensitivity).”
Quote in the paperSubstantial claimMay combine two claims.
Findingown dataThe final change in the shallow convection introduces the largest change, although it brings CAM5 closer to the original CAM4 in some variables.
“The final change in the shallow convection introduces the largest change (last step in panel c), although it brings CAM5 closer to the original CAM4 in some variables (panel b).”
Quote in the paperNot a substantial claimMay combine two claims.
InterpretationreasoningThe CMIP5 models are neither independent of each other nor independent of the earlier generation of models.
“thus supporting an earlier hypothesis that the models in the new ensemble are neither independent of each other nor independent of the earlier generation”
Quote in the paperSubstantial claimMay combine two claims.
InterpretationreasoningThe results point to remarkable consistency and robustness in many aspects of simulated present-day and future climate, but also suggest that convergence to reality is slow and radical breakthroughs are hard to achieve.
“The results point to a remarkable consistency and robustness in many aspects of simulated present day and future climate, but it also suggests that convergence to reality is slow and radical breakthroughs are hard to achieve.”
Quote in the paperSubstantial claimProbably not a substantial claim: may not pass S2 (checkable), S4 (based).
Interpretationnone givenConfidence is greatest in those aspects of climate change that we understand and can link back to known physical processes and simpler models and concepts.
“Confidence is greatest in those aspects of climate change that we understand and can link back to known physical processes and simpler models and concepts (e.g., the global energy balance).”
Quote in the paperNot a substantial claimProbably not a substantial claim: may not pass S2 (checkable).
InterpretationreasoningTransparency in the model development process is helpful in understanding model evaluation and projections.
“We argue that transparency in the model development process is helpful in understanding model evaluation and projections and contributes to that insight.”
Quote in the paperNot a substantial claimClassified as probably not a substantial claim. May combine two claims.
Study design and conductnone givenAll results are based only on model output and assume no knowledge about the structure, parameterizations, or code of any model.
“Note that all results presented here are only based on model output; they assume no knowledge about the structure, parameterizations, or code of any model.”
Quote in the paperSubstantial claimProbably not a substantial claim: may not pass S4 (based).
Study design and conductnone givenThe methodological choices made for the similarity metric do not affect the main conclusions.
“None of those choices affect the main conclusions.”
Quote in the paperNot a substantial claimProbably not a substantial claim: may not pass S2 (checkable). May combine two claims.
InterpretationreasoningConfidence in model projections does not come from the sheer amount of code and data and cannot be demonstrated by repeated verification.
“Confidence in model projections does not come from the sheer amount of code and data and cannot be demonstrated by repeated verification.”
Quote in the paperNot a substantial claimMay combine two claims.
PremisecitationLinking model performance metrics to model quality or skill is difficult, subjective, and strongly metric dependent.
“but with the strong caveat that linking model performance metrics to model quality or skill is difficult, subjective, and strongly metric dependent [Gleckler et al., 2008]”
Quote in the paperSubstantial claim0 of 1 sources checked- cites Gleckler et al., 2008
Not checked in the free run.
Probably not a substantial claim: may not pass S4 (based).
Interpretationnone givenOne reason some models are so similar is because they share common code.
“We propose that one reason some models are so similar is because they share common code.”
Quote in the paperNot a substantial claimClassified as probably not a substantial claim.
PremisecitationModel similarities result from models evolving from their ancestors by modification and by exchange of ideas and code with other groups.
“MK11 argued that such similarities result from the fact that models evolve from their ancestors by modification and by exchange of ideas and code with other groups.”
Quote in the paperSubstantial claim0 of 1 sources checked- cites Masson and Knutti, 2011
Not checked in the free run.
The authors state this as an assumption.
The models in an ensemble are approximately a representative sample of uncertainty in how to best describe the climate system given limited observations, imperfect understanding, and finite computational resources.
“This assumes that the models are approximately a representative sample of our uncertainty in how to best describe the climate system given limited observations, imperfect understanding, and finite computational resources [Knutti, 2008;Yokohata et al., 2012].”
The authors state this as an assumption.
There are not too many similarities among models that would bias the results of an ensemble.
“It also assumes that there are not too many similarities that would bias the results.”
Claims other papers make about this one
Each is checked against this paper’s own text: does it say what the citing paper says it does?
CMIP5 projections are an incremental advance over CMIP3 data, so using CMIP3 does not limit the relevance of the analysis.
“Since CMIP5 projections are an incremental advance over CMIP3 data [34–36], this does not limit the relevance of our analysis as a tool for assessing anthropogenic influences on future fire activity.”
From Incorporating Anthropogenic Influences into Fire Probability Models: Effects of Human Activity and Climate Change on Fire Activity in California (2016) · cites this paper as [34]
Self-check
Percentages, sums and reported differences re-computed from the paper’s own numbers.
Each contradiction between two passages listed here was confirmed by an independent check.
Overall distance metric is described two different ways
MinorThe methods section says the combined temperature-precipitation distance used for Figure 3 is a mean square, while the Figure 3 caption calls it a root mean square. Taking the square root changes the reported distance values.
“for Figures 1 and 3, the metric now also includes differences in the annual mean climatology and that we use the mean square of the temperature and precipitation distance to define overall similarity”
“The distance metric is calculated as the root mean square of the surface temperature and precipitation distance as in Figure 1”
Cites
Climate change 2007: the physical science basis
Solomon, S., Qin, D., Manning, M., Marquis, M. C., Averyt, K. B., Tignor, M., Miller, H. L., & Chen, Z. (2007) · Cited by 23,398 · see citing works
An Overview of CMIP5 and the Experiment Design
Taylor, K. E., Stouffer, R. J., & Meehl, G. A. (2012) · Bulletin of the American Meteorological Society · doi:10.1175/bams-d-11-00094.1 · Cited by 14,052 · see citing works
The use of the multi-model ensemble in probabilistic climate projections
Tebaldi, C., & Knutti, R. (2007) · Philosophical Transactions of the Royal Society A: Mathematical, Physical and Engineering Sciences · doi:10.1098/rsta.2007.2076 · Cited by 1,862 · see citing works
Self-citationRobustness and uncertainties in the new CMIP5 climate model projections
Knutti, R., & Sedláček, J. (2013) · Nature Climate Change · doi:10.1038/nclimate1716 · Cited by 1,569 · see citing works
Self-citationPerformance metrics for climate models.
Gleckler, P. J., Taylor, K. E., & Doutriaux, C. (2008) · Journal of Geophysical Research: Atmospheres · doi:10.1029/2007jd008972 · Cited by 1,328 · see citing works
Challenges in combining projections from multiple climate models.
Knutti, R., Furrer, R., Tebaldi, C., Cermak, J., & Meehl, G. A. (2010) · Journal of Climate · doi:10.1175/2009jcli3361.1 · Cited by 1,270 · see citing works
Self-citationA numerical method for the study of the circulation of the world ocean
Bryan, K. (1969) · Journal of Computational Physics · doi:10.1016/0021-9991(69)90004-7 · Cited by 974 · see citing works
A Numerical Method for the Study of the Circulation of the World Ocean
Bryan, K. (1997) · Journal of Computational Physics · doi:10.1006/jcph.1997.5699 · Cited by 906 · see citing works
How Well Do Coupled Models Simulate Today's Climate?
Reichler, T. J., & Kim, J. (2008) · Bulletin of the American Meteorological Society · doi:10.1175/bams-89-3-303 · Cited by 880 · see citing works
Risks of Model Weighting in Multimodel Climate Projections
Weigel, A. P., Knutti, R., Liniger, M. A., & Appenzeller, C. (2010) · Journal of Climate · doi:10.1175/2010jcli3594.1 · Cited by 386 · see citing works
Self-citationMasson, D., & Knutti, R. (2011) · Geophysical Research Letters · doi:10.1029/2011gl046864 · Cited by 354 · see citing works
Self-citationA Summary of the CMIP5 Experiment Design
Taylor, K. E., Stouffer, R. J., Meehl, G. A., Cox, P. M., Eyring, V., Flato, G. M., Gillett, N. P., Giorgetta, M. A., Bala, G., Hazeleger, W., et al. (2010) · Cited by 333 · see citing works
Should we believe model predictions of future climate change?
Knutti, R. (2008) · Philosophical Transactions of the Royal Society A: Mathematical, Physical and Engineering Sciences · doi:10.1098/rsta.2008.0169 · Cited by 279 · see citing works
Self-citationThe Evolution of Climate Sensitivity and Climate Feedbacks in the Community Atmosphere Model
Gettelman, A., Kay, J. E., & Shell, K. M. (2011) · Journal of Climate · doi:10.1175/jcli-d-11-00197.1 · Cited by 161 · see citing works
Self-citationReliability of multi-model and structurally different single-model ensembles
Yokohata, T., Annan, J. D., Collins, M. D., Jackson, C. S., Tobis, M., Webb, M. J., & Hargreaves, J. C. (2011) · Climate Dynamics · doi:10.1007/s00382-011-1203-1 · Cited by 58 · see citing works
Using a Multiphysics Ensemble for Exploring Diversity in Cloud–Shortwave Feedback in GCMs
Watanabe, M., Shiogama, H., Yokohata, T., Kamae, Y., Yoshimori, M., Ogura, T., Annan, J. D., Hargreaves, J. C., Emori, S., & Kimoto, M. (2012) · Journal of Climate · doi:10.1175/jcli-d-11-00564.1 · Cited by 34 · see citing works
Flagged first, then by citations
Cited by
Sorted by citations
The Community Earth System Model Version 2 (CESM2)
Danabasoglu, G., Lamarque, J., Bacmeister, J. T., Bailey, D. A., DuVivier, A. K., Edwards, J., Emmons, L. K., Fasullo, J., García, R. R., Gettelman, A., et al. (2020) · Journal of Advances in Modeling Earth Systems · doi:10.1029/2019ms001916 · Cited by 3,273 · see citing works
Self-citationKay, J. E., Deser, C., Phillips, A. S., Mai, A., Hannay, C., Strand, G., Arblaster, J. M., Bates, S. C., Gokhan Danabasoglu, C., Edwards, J., et al. (2014) · Bulletin of the American Meteorological Society · doi:10.1175/bams-d-13-00255.1 · Cited by 2,496 · see citing works
Causes of Higher Climate Sensitivity in CMIP6 Models
Zelinka, M. D., Myers, T. A., McCoy, D. T., Po–Chedley, S., Caldwell, P., Ceppi, P., Klein, S. A., & Taylor, K. E. (2020) · Geophysical Research Letters · doi:10.1029/2019gl085782 · Cited by 1,758 · see citing works
Wang, T., Hamann, A., Spittlehouse, D., & Carroll, C. (2016) · PLoS ONE · doi:10.1371/journal.pone.0156720 · Cited by 1,110 · see citing works
Atmospheric circulation as a source of uncertainty in climate change projections
Shepherd, T. G. (2014) · Nature Geoscience · doi:10.1038/ngeo2253 · Cited by 1,062 · see citing works
Séférian, R., Nabat, P., Michou, M., Saint‐Martin, D., Voldoire, A., Colin, J., Decharme, B., Delire, C., Berthet, S., Chevallier, M., et al. (2019) · Journal of Advances in Modeling Earth Systems · doi:10.1029/2019ms001791 · Cited by 925 · see citing works
Near-term Climate Change: Projections and Predictability
Change, I. P. O. C. (2014) · Cambridge University Press eBooks · doi:10.1017/cbo9781107415324.023 · Cited by 927 · see citing works
Kwiatkowski, L., Torres, O., Bopp, L., Aumont, O., Chamberlain, M., Christian, J. R., Dunne, J. P., Gehlen, M., Ilyina, T., John, J. G., et al. (2020) · Biogeosciences · doi:10.5194/bg-17-3439-2020 · Cited by 897 · see citing works
Observed heavy precipitation increase confirms theory and early models
Fischer, E. M., & Knutti, R. (2016) · Nature Climate Change · doi:10.1038/nclimate3110 · Cited by 772 · see citing works
Self-citationShepherd, T. G., Boyd, E., Calel, R. A., Chapman, S. C., Dessai, S., Dima, I. M., Fowler, H. J., James, R., Maraun, D., Martius, O., et al. (2018) · Climatic Change · doi:10.1007/s10584-018-2317-9 · Cited by 800 · see citing works
Causes, impacts and patterns of disastrous river floods
Merz, B., Blöschl, G., Vorogushyn, S., Dottori, F., Aerts, J. C. J. H., Bates, P., Bertola, M., Kemter, M., Kreibich, H., Lall, U., et al. (2021) · Nature Reviews Earth & Environment · doi:10.1038/s43017-021-00195-3 · Cited by 741 · see citing works
Past warming trend constrains future warming in CMIP6 models
Tokarska, K. B., Stolpe, M. B., Sippel, S., Fischer, E. M., Smith, C., Lehner, F., & Knutti, R. (2020) · Science Advances · doi:10.1126/sciadv.aaz9549 · Cited by 749 · see citing works
Self-citationConfiguration and assessment of the GISS ModelE2 contributions to the CMIP5 archive
Schmidt, G. A., Kelley, M., Nazarenko, L., Ruedy, R. A., Russell, G. L., Aleinov, I., Bauer, M., Bauer, S. E., Bhat, M. K., Bleck, R., et al. (2014) · Journal of Advances in Modeling Earth Systems · doi:10.1002/2013ms000265 · Cited by 714 · see citing works
Dominance of the Southern Ocean in Anthropogenic Carbon and Heat Uptake in CMIP5 Models
Frölicher, T. L., Sarmiento, J. L., Paynter, D. J., Dunne, J. P. P., Krasting, J. P., & Winton, M. (2014) · Journal of Climate · doi:10.1175/jcli-d-14-00117.1 · Cited by 682 · see citing works
GISS‐E2.1: Configurations and Climatology
Kelley, M., Schmidt, G. A., Nazarenko, L., Bauer, S. E., Ruedy, R. A., Russell, G. L., Ackerman, A. S., Aleinov, I., Bauer, M., Bleck, R., et al. (2020) · Journal of Advances in Modeling Earth Systems · doi:10.1029/2019ms002025 · Cited by 672 · see citing works
Partitioning climate projection uncertainty with multiple large ensembles and CMIP5/6
Lehner, F., Deser, C., Maher, N., Marotzke, J., Fischer, E. M., Brunner, L., Knutti, R., & Hawkins, E. (2020) · Earth System Dynamics · doi:10.5194/esd-11-491-2020 · Cited by 701 · see citing works
Self-citationA climate model projection weighting scheme accounting for performance and interdependence
Knutti, R., Sedláčék, J., Sanderson, B. M., Lorenz, R., Fischer, E. M., & Eyring, V. (2017) · Geophysical Research Letters · doi:10.1002/2016gl072012 · Cited by 501 · see citing works
Self-citationHigh Climate Sensitivity in the Community Earth System Model Version 2 (CESM2)
Gettelman, A., Hannay, C., Bacmeister, J. T., Neale, R., Pendergrass, A. G., Danabasoglu, G., Lamarque, J., Fasullo, J., Bailey, D. A., Lawrence, D. M., et al. (2019) · Geophysical Research Letters · doi:10.1029/2019gl083978 · Cited by 491 · see citing works
Self-citationLarge loss of CO2 in winter observed across the northern permafrost region
Natali, S. M., Watts, J. D., Rogers, B. M., Potter, S., Ludwig, S., Selbmann, A. K., Sullivan, P. F., Abbott, B. W., Arndt, K. A., Birch, L., et al. (2019) · Nature Climate Change · doi:10.1038/s41558-019-0592-8 · Cited by 454 · see citing works
Progressing emergent constraints on future climate change
Hall, A. D., Cox, P. M., Huntingford, C., & Klein, S. A. (2019) · Nature Climate Change · doi:10.1038/s41558-019-0436-6 · Cited by 462 · see citing works
Integrated Risk and Uncertainty Assessment of Climate Change Response Policies
Change, I. P. O. C. (2015) · Cambridge University Press eBooks · doi:10.1017/cbo9781107415416.008 · Cited by 415 · see citing works
A Representative Democracy to Reduce Interdependency in a Multimodel Ensemble
Sanderson, B. M., Knutti, R., & Caldwell, P. (2015) · Journal of Climate · doi:10.1175/jcli-d-14-00362.1 · Cited by 411 · see citing works
Self-citationClimate change reduces extent of temperate drylands and intensifies drought in deep soils
Schlaepfer, D. R., Bradford, J. B., Lauenroth, W. K., Munson, S. M., Tietjen, B., Hall, S. A., Wilson, S. D., Duniway, M. C., Jia, G., Pyke, D. A., et al. (2017) · Nature Communications · doi:10.1038/ncomms14196 · Cited by 391 · see citing works
Lutz, A., ter Maat, H. W., Biemans, H., Shrestha, A. B., Wester, P., & Immerzeel, W. W. (2016) · International Journal of Climatology · doi:10.1002/joc.4608 · Cited by 382 · see citing works
Reduced global warming from CMIP6 projections when weighting models by performance and independence
Brunner, L., Pendergrass, A. G., Lehner, F., Merrifield, A. L., Lorenz, R., & Knutti, R. (2020) · Earth System Dynamics · doi:10.5194/esd-11-995-2020 · Cited by 386 · see citing works
Self-citation(IPCC), I. P. O. C. C. (2023) · Cambridge University Press eBooks · doi:10.1017/9781009157896.003 · Cited by 382 · see citing works
Greater future global warming inferred from Earth’s recent energy budget
Brown, P. T., & Caldeira, K. (2017) · Nature · doi:10.1038/nature24672 · Cited by 334 · see citing works
Beyond equilibrium climate sensitivity
Knutti, R., Rugenstein, M. A. A., & Hegerl, G. C. (2017) · Nature Geoscience · doi:10.1038/ngeo3017 · Cited by 344 · see citing works
Self-citationZhou, B., Wen, Q. H., Xu, Y., Song, L., & Zhang, X. (2014) · Journal of Climate · doi:10.1175/jcli-d-13-00761.1 · Cited by 333 · see citing works
Long‐term ozone changes and associated climate impacts in CMIP5 simulations
Eyring, V., Arblaster, J. M., Cionni, I., Sedláčék, J., Perlwitz, J., Young, P. J., Bekki, S., Bergmann, D., Cameron-Smith, P. J., Collins, W. J., et al. (2013) · Journal of Geophysical Research Atmospheres · doi:10.1002/jgrd.50316 · Cited by 326 · see citing works
Snowfall less sensitive to warming in Karakoram than in Himalayas due to a unique seasonal cycle
Kapnick, S., Delworth, T. L., Ashfaq, M., Malyshev, S. L., & Milly, P. C. D. (2014) · Nature Geoscience · doi:10.1038/ngeo2269 · Cited by 314 · see citing works
Ahmed, K., Sachindra, D. A., Shahid, S., Demirel, M. C., & Chung, . (2019) · Hydrology and earth system sciences · doi:10.5194/hess-23-4803-2019 · Cited by 311 · see citing works
Evaluation of CMIP5 20th century climate simulations for the Pacific Northwest USA
Rupp, D. E., Abatzoglou, J. T., Hegewisch, K. C., & Mote, P. W. (2013) · Journal of Geophysical Research Atmospheres · doi:10.1002/jgrd.50843 · Cited by 308 · see citing works
Alexander, M. A., Scott, J. D., Friedland, K. D., Mills, K. E., Nye, J. A., Pershing, A. J., & Thomas, A. C. (2018) · Elementa Science of the Anthropocene · doi:10.1525/elementa.191 · Cited by 301 · see citing works
Making climate projections conditional on historical observations
Ribes, A., Qasmi, S., & Gillett, N. P. (2021) · Science Advances · doi:10.1126/sciadv.abc0671 · Cited by 297 · see citing works
Characterizing Uncertainty of the Hydrologic Impacts of Climate Change
Clark, M., Wilby, R. L., Gutmann, E. D., Vano, J. A., Gangopadhyay, S., Wood, A. W., Fowler, H. J., Prudhomme, C., Arnold, J. R., & Brekke, L. D. (2016) · Current Climate Change Reports · doi:10.1007/s40641-016-0034-x · Cited by 299 · see citing works
Storylines of Atmospheric Circulation Change for European Regional Climate Impact Assessment
Zappa, G., & Shepherd, T. G. (2017) · Journal of Climate · doi:10.1175/jcli-d-16-0807.1 · Cited by 288 · see citing works
Arnell, N. W., & Lloyd-Hughes, B. (2013) · Climatic Change · doi:10.1007/s10584-013-0948-4 · Cited by 283 · see citing works
A Common Framework for Approaches to Extreme Event Attribution
Shepherd, T. G. (2016) · Current Climate Change Reports · doi:10.1007/s40641-016-0033-y · Cited by 289 · see citing works
Pattern scaling: Its strengths and limitations, and an update on the latest model simulations
Tebaldi, C., & Arblaster, J. M. (2014) · Climatic Change · doi:10.1007/s10584-013-1032-9 · Cited by 274 · see citing works
Krueger, S. K., Fu, Q., Liou, K. N., & Chin, H.-N. S. (1995) · Journal of applied meteorology · doi:10.1175/1520-0450-34.1.281 · Cited by 262 · see citing works
Herman, J. D., Quinn, J. D., Steinschneider, S., Giuliani, M., & Fletcher, S. M. (2020) · Water Resources Research · doi:10.1029/2019wr025502 · Cited by 268 · see citing works
Robust ecological drought projections for drylands in the 21st century
Bradford, J. B., Schlaepfer, D. R., Lauenroth, W. K., & Palmquist, K. A. (2020) · Global Change Biology · doi:10.1111/gcb.15075 · Cited by 245 · see citing works
Regional Climate Sensitivity of Climate Extremes in CMIP6 Versus CMIP5 Multimodel Ensembles
Seneviratne, S. I., & Hauser, M. (2020) · Earth s Future · doi:10.1029/2019ef001474 · Cited by 242 · see citing works
Skill and independence weighting for multi-model assessments
Sanderson, B. M., Wehner, M. F., & Knutti, R. (2017) · Geoscientific model development · doi:10.5194/gmd-10-2379-2017 · Cited by 251 · see citing works
Self-citationEvaluating the Performance of Past Climate Model Projections
Hausfather, Z., Drake, H. F., Abbott, T. H., & Schmidt, G. A. (2019) · Geophysical Research Letters · doi:10.1029/2019gl085378 · Cited by 238 · see citing works
Simulations for CMIP6 With the AWI Climate Model AWI‐CM‐1‐1
Semmler, T., Danilov, S. D., Gierz, P., Goessling, H., Hegewald, J., Hinrichs, C., Koldunov, N., Khosravi, N., Mu, L., Rackow, T., et al. (2020) · Journal of Advances in Modeling Earth Systems · doi:10.1029/2019ms002009 · Cited by 243 · see citing works
Models agree on forced response pattern of precipitation and temperature extremes
Fischer, E. M., Sedláčék, J., Hawkins, E., & Knutti, R. (2014) · Geophysical Research Letters · doi:10.1002/2014gl062018 · Cited by 229 · see citing works
Self-citationThe effects of 1.5 and 2 degrees of global warming on Africa in the CORDEX ensemble
Nikulin, G., Lennard, C., Dosio, A., Kjellström, E., Chen, Y., Haensler, A., Kupiainen, M., Laprise, R., Mariotti, L., Maule, C. F., et al. (2018) · Environmental Research Letters · doi:10.1088/1748-9326/aab1b1 · Cited by 218 · see citing works
Evaluation of CMIP6 GCM rainfall in mainland Southeast Asia
Iqbal, Z., Shahid, S., Ahmed, K., Ismail, T., Ziarh, G. F., Chung, ., & Wang, X. (2021) · Atmospheric Research · doi:10.1016/j.atmosres.2021.105525 · Cited by 215 · see citing works
Ghan, S. J., Wang, M., Zhang, S., Ferrachat, S., Gettelman, A., Griesfeller, J., Kipling, Z., Lohmann, U., Morrison, H., Neubauer, D., et al. (2016) · Proceedings of the National Academy of Sciences · doi:10.1073/pnas.1514036113 · Cited by 210 · see citing works
Self-citationAbramowitz, G., Herger, N., Gutmann, E. D., Hammerling, D., Knutti, R., Leduc, M., Lorenz, R., Pincus, R. L., & Schmidt, G. A. (2019) · Earth System Dynamics · doi:10.5194/esd-10-91-2019 · Cited by 224 · see citing works
Self-citationSources of uncertainties in 21st century projections of potential ocean ecosystem stressors
Frölicher, T. L., Rodgers, K. B., Stock, C. A. A., & Cheung, W. W. L. (2016) · Global Biogeochemical Cycles · doi:10.1002/2015gb005338 · Cited by 205 · see citing works
On the spread of changes in marine low cloud cover in climate model simulations of the 21st century
Qu, X., Hall, A. D., Klein, S. A., & Caldwell, P. (2013) · Climate Dynamics · doi:10.1007/s00382-013-1945-z · Cited by 208 · see citing works
Tietjen, B., Schlaepfer, D. R., Bradford, J. B., Lauenroth, W. K., Hall, S. A., Duniway, M. C., Hochstrasser, T., Jia, G., Munson, S. M., Pyke, D. A., et al. (2016) · Global Change Biology · doi:10.1111/gcb.13598 · Cited by 195 · see citing works
Salman, S. A., Shahid, S., Ismail, T., Ahmed, K., & Wang, X.-J. (2018) · Atmospheric Research · doi:10.1016/j.atmosres.2018.07.008 · Cited by 178 · see citing works
High-resolution monthly precipitation and temperature time series from 2006 to 2100
Karger, D. N., Schmatz, D. R., Dettling, G., & Zimmermann, N. E. (2020) · Scientific Data · doi:10.1038/s41597-020-00587-y · Cited by 194 · see citing works
Li, M., Cao, X., Liu, D., Fu, Q., Li, T., & Shang, R. (2021) · Agricultural Water Management · doi:10.1016/j.agwat.2021.107235 · Cited by 202 · see citing works
Global warming accelerates soil heterotrophic respiration
Nissan, A., Alcolombri, U., Peleg, N., Galili, N., Jiménez‐Martínez, J., Molnár, P., & Holzner, M. (2023) · Nature Communications · doi:10.1038/s41467-023-38981-w · Cited by 195 · see citing works
Myhre, G., Forster, P. M. D. F., Samset, B. H., Hodnebrog, Ø., Sillmann, J., Aalbergsjø, S. G., Andrews, T., Boucher, O., Faluvegi, G., Fläschner, D., et al. (2016) · Bulletin of the American Meteorological Society · doi:10.1175/bams-d-16-0019.1 · Cited by 189 · see citing works
Khan, N., Shahid, S., Ahmed, K., Ismail, T., Nawaz, N., & Son, M. (2018) · Water · doi:10.3390/w10121793 · Cited by 155 · see citing works
Addressing Interdependency in a Multimodel Ensemble by Interpolation of Model Properties
Sanderson, B. M., Knutti, R., & Caldwell, P. (2015) · Journal of Climate · doi:10.1175/jcli-d-14-00361.1 · Cited by 185 · see citing works
Self-citationA closer look at novel climates: new methods and insights at continental to landscape scales
Mahony, C. R., Cannon, A. J., Wang, T., & Aitken, S. N. (2017) · Global Change Biology · doi:10.1111/gcb.13645 · Cited by 178 · see citing works
Manzini, E., Karpechko, A. Y., Anstey, J. A., Baldwin, M., Black, R. X., Cagnazzo, C., Calvo, N., Charlton-Perez, A. J., Christiansen, B., Davini, P., et al. (2014) · Journal of Geophysical Research Atmospheres · doi:10.1002/2013jd021403 · Cited by 177 · see citing works
Massimi, M. (2022) · doi:10.1093/oso/9780197555620.001.0001 · Cited by 182 · see citing works
Selecting a climate model subset to optimise key ensemble properties
Herger, N., Abramowitz, G., Knutti, R., Angélil, O., Lehmann, K., & Sanderson, B. M. (2018) · Earth System Dynamics · doi:10.5194/esd-9-135-2018 · Cited by 177 · see citing works
Self-citationClassification of CMIP5 Future Climate Responses by the Tropical Sea Surface Temperature Changes
Mizuta, R., Arakawa, O., Ose, T., Kusunoki, S., Endo, H., & Kitoh, A. (2014) · SOLA · doi:10.2151/sola.2014-035 · Cited by 170 · see citing works
Pour, S. H., Shahid, S., Chung, E.-S., & Wang, X.-J. (2018) · Atmospheric Research · doi:10.1016/j.atmosres.2018.06.006 · Cited by 183 · see citing works
Hadley cell expansion in CMIP6 models
Grise, K. M., & Davis, S. (2020) · Atmospheric chemistry and physics · doi:10.5194/acp-20-5249-2020 · Cited by 166 · see citing works
Practice and philosophy of climate model tuning across six US modeling centers
Schmidt, G. A., Bader, D. C., Donner, L. J., Elsaesser, G. S., Golaz, J., Hannay, C., Molod, A. M., Neale, R., & Saha, S. (2017) · Geoscientific model development · doi:10.5194/gmd-10-3207-2017 · Cited by 164 · see citing works
The Southern Ocean in the Coupled Model Intercomparison Project phase 5
Meijers, A. (2014) · Philosophical Transactions of the Royal Society A Mathematical Physical and Engineering Sciences · doi:10.1098/rsta.2013.0296 · Cited by 162 · see citing works
Cannon, A. J. (2014) · Journal of Climate · doi:10.1175/jcli-d-14-00636.1 · Cited by 160 · see citing works
The potential to reduce uncertainty in regional runoff projections from climate models
Lehner, F., Wood, A. W., Vano, J. A., Lawrence, D. M., Clark, M., & Mankin, J. (2019) · Nature Climate Change · doi:10.1038/s41558-019-0639-x · Cited by 160 · see citing works
Liang, Y., Gillett, N. P., & Monahan, A. H. (2020) · Geophysical Research Letters · doi:10.1029/2019gl086757 · Cited by 160 · see citing works
Davini, P., & D’Andrea, F. (2016) · Journal of Climate · doi:10.1175/jcli-d-16-0242.1 · Cited by 154 · see citing works
Statistical significance of climate sensitivity predictors obtained by data mining
Caldwell, P. M., Bretherton, C. S., Zelinka, M. D., Klein, S. A., Santer, B. D., & Sanderson, B. M. (2014) · Geophysical Research Letters · doi:10.1002/2014gl059205 · Cited by 153 · see citing works
Design considerations for riverine floods in a changing climate – A review
François, B., Schlef, K., Wi, S., & Brown, C. (2019) · Journal of Hydrology · doi:10.1016/j.jhydrol.2019.04.068 · Cited by 154 · see citing works
Zhang, J., Guan, K., Peng, B., Pan, M., Zhou, W. M., Jiang, C., Kimm, H., Franz, T. E., Grant, R. F., Yang, Y., et al. (2021) · Nature Communications · doi:10.1038/s41467-021-25254-7 · Cited by 153 · see citing works
Mann, M. L., Batllori, E., Moritz, M. A., Waller, E. K., Berck, P., Flint, A. L., Flint, L. E., & Dolfi, E. (2016) · PLOS ONE · doi:10.1371/journal.pone.0153589 · Cited by 151 · see citing works
Telteu, C.-E., Schmied, H. M., Thiery, W., Leng, G., Burek, P., Liu, X., Boulangé, J., Andersen, L. S., Grillakis, M. G., Gosling, S. N., et al. (2021) · Geoscientific model development · doi:10.5194/gmd-14-3843-2021 · Cited by 151 · see citing works
Palazzi, E., Filippi, L., & von Hardenberg, J. (2016) · Climate Dynamics · doi:10.1007/s00382-016-3316-z · Cited by 152 · see citing works
Biotic and Climatic Velocity Identify Contrasting Areas of Vulnerability to Climate Change
Carroll, C., Lawler, J. J., Roberts, D. R., & Hamann, A. (2015) · PLOS ONE · doi:10.1371/journal.pone.0140486 · Cited by 143 · see citing works
Mülmenstädt, J., & Feingold, G. (2018) · Current Climate Change Reports · doi:10.1007/s40641-018-0089-y · Cited by 159 · see citing works
Exploring, exploiting and evolving diversity of aquatic ecosystem models: a community perspective
Janssen, A. B. G., Arhonditsis, G. B., Beusen, A. H. W., Bolding, K., Bruce, L. C., Bruggeman, J., Couture, R., Downing, A. S., Elliott, J. A., Frassl, M. A., et al. (2015) · Aquatic Ecology · doi:10.1007/s10452-015-9544-1 · Cited by 146 · see citing works
Bradford, J. B., & Bell, D. M. (2017) · Frontiers in Ecology and the Environment · doi:10.1002/fee.1445 · Cited by 144 · see citing works
Prestoration: using species in restoration that will persist now and into the future
Butterfield, B. J., Copeland, S. M., Munson, S. M., Roybal, C. M., & Wood, T. E. (2016) · Restoration Ecology · doi:10.1111/rec.12381 · Cited by 139 · see citing works
Impact of climate change on pavement structural performance in the United States
Gudipudi, P. P., Underwood, B. S., & Zalghout, A. A. (2017) · Transportation Research Part D Transport and Environment · doi:10.1016/j.trd.2017.09.022 · Cited by 137 · see citing works
Northern Hemisphere vegetation change drives a Holocene thermal maximum
Thompson, A. J., Zhu, J., Poulsen, C. J., Tierney, J. E., & Skinner, C. B. (2022) · Science Advances · doi:10.1126/sciadv.abj6535 · Cited by 137 · see citing works
Beusch, L., Gudmundsson, L., & Seneviratne, S. I. (2020) · Earth System Dynamics · doi:10.5194/esd-11-139-2020 · Cited by 136 · see citing works
Comparison of past and future simulations of ENSO in CMIP5/PMIP3 and CMIP6/PMIP4 models
Brown, J. R., Brierley, C., An, S., Guarino, M. V., Stevenson, S. L., Williams, C. J. R., Zhang, Q., Zhao, A., Abe‐Ouchi, A., Braconnot, P., et al. (2020) · Climate of the past · doi:10.5194/cp-16-1777-2020 · Cited by 148 · see citing works
Hydrological response to climate change: The Pearl River, China under different RCP scenarios
Yan, D., Werners, S. E., Ludwig, F., & Huang, H. Q. (2015) · Journal of Hydrology Regional Studies · doi:10.1016/j.ejrh.2015.06.006 · Cited by 133 · see citing works
Evaluating Emergent Constraints on Equilibrium Climate Sensitivity
Caldwell, P., Zelinka, M. D., & Klein, S. A. (2018) · Journal of Climate · doi:10.1175/jcli-d-17-0631.1 · Cited by 132 · see citing works
Brunner, L., Lorenz, R., Zumwald, M., & Knutti, R. (2019) · Environmental Research Letters · doi:10.1088/1748-9326/ab492f · Cited by 137 · see citing works
Self-citationSpringer, Y. P., Jarnevich, C. S., Barnett, D. T., Monaghan, A. J., & Eisen, R. J. (2015) · American Journal of Tropical Medicine and Hygiene · doi:10.4269/ajtmh.15-0330 · Cited by 129 · see citing works
Fast and slow responses of Southern Ocean sea surface temperature to SAM in coupled climate models
Kostov, Y., Marshall, J., Hausmann, U., Armour, K. C., Ferreira, D., & Holland, M. M. (2017) · Climate Dynamics · doi:10.1007/s00382-016-3162-z · Cited by 129 · see citing works
Quinn, J. D., Reed, P. M., Giuliani, M., Castelletti, A. F., Oyler, J. W., & Nicholas, R. E. (2018) · Water Resources Research · doi:10.1029/2018wr022743 · Cited by 129 · see citing works
Brient, F. (2019) · Advances in Atmospheric Sciences · doi:10.1007/s00376-019-9140-8 · Cited by 137 · see citing works
ClimateEU, scale-free climate normals, historical time series, and future projections for Europe
Marchi, M., Castellanos‐Acuña, D., Hamann, A., Wang, T., Ray, D., & Menzel, A. (2020) · Scientific Data · doi:10.1038/s41597-020-00763-0 · Cited by 131 · see citing works
Fasullo, J., & Nerem, R. S. (2018) · Proceedings of the National Academy of Sciences · doi:10.1073/pnas.1813233115 · Cited by 125 · see citing works
CMIP5 model selection for ISMIP6 ice sheet model forcing: Greenland and Antarctica
Barthel, A. M., Agosta, C., Little, C. M., Hattermann, T., Jourdain, N. C., Goelzer, H., Nowicki, S., Seroussi, H. L., Straneo, F., & Bracegirdle, T. J. (2020) · The Cryosphere · doi:10.5194/tc-14-855-2020 · Cited by 125 · see citing works
- Authors
- Knutti, R., Masson, D., & Gettelman, A.
- Affiliations
- ETH Zurich (CH)
- Federal Office of Meteorology and Climatology MeteoSwiss (CH)
- NSF National Center for Atmospheric Research (US)
- Corresponding author
- Knutti, Reto
- Venue
- Geophysical Research Letters
- Publisher
- American Geophysical Union (AGU)
- Published
- 2013-03-26
- Volume
- 40
- Issue
- 6
- Pages
- 1194-1199
- ISSN
- 0094-8276 (ISSN-L)
- 1944-8007
- OpenAlex
- W1796961055
- Semantic Scholar
- f6507ca951e61214c9268ce9a43376724b2f9bcf
- Cited by
- 918
- References
- 17
- Citations by year
- 2026: 37 · 2025: 42 · 2024: 54 · 2023: 73 · 2022: 114 · 2021: 126 · 2020: 109 · 2019: 64 · 2018: 76 · 2017: 67 · 2016: 51 · 2015: 55 · 2014: 42 · 2013: 7
- FWCI
- 39.41
- Type
- journal article
- Language
- en
- Open access
- bronze
- doi.org
- Locations
- Geophysical Research Letters (publishedVersion)
- Repository for Publications and Research Data (ETH Zurich) (submittedVersion, other-oa)
- ETH Zürich Research Collection
- Topics
- Physical Sciences › Environmental Science › Global and Planetary Change › Climate variability and models
- Physical Sciences › Earth and Planetary Sciences › Atmospheric Science › Meteorological Phenomena and Simulations
- Social Sciences › Economics, Econometrics and Finance › Economics and Econometrics › Climate Change Policy and Economics
- Keywords
- CMIP5, multi-model ensemble, model validation against observations, climate change projections, statistical model comparison
About these checks
Registry, retraction, Cites and statistics results are computed, not judged, with one exception: a printed reference that no index lists is read once by a model before it counts as a citation error. Claims are extracted by a model and kept only when their quote appears verbatim in the text; each cited source is then checked, with a model’s help, for whether it says what the claim relies on. Those verdicts can be wrong — read the claim’s quote and the cited source before relying on one.
Claims read by deepseek-v4.1-flash under definition version 3 (extract-v3) on 2026-10-06.
Classified by jev-1.13-20260917 (gold-guideline-v0.2) on 2026-10-06.
Statistics and arithmetic are recomputed, not judged.
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