Articles | Volume 9, issue 4
https://doi.org/10.5194/esd-9-1235-2018
© Author(s) 2018. This work is distributed under
the Creative Commons Attribution 4.0 License.
the Creative Commons Attribution 4.0 License.
https://doi.org/10.5194/esd-9-1235-2018
© Author(s) 2018. This work is distributed under
the Creative Commons Attribution 4.0 License.
the Creative Commons Attribution 4.0 License.
Simulation of observed climate changes in 1850–2014 with climate model INM-CM5
Evgeny Volodin
CORRESPONDING AUTHOR
Institute for Numerical Mathematics, INM RAS, Gubkina 8, Moscow 119333, Russia
Andrey Gritsun
Institute for Numerical Mathematics, INM RAS, Gubkina 8, Moscow 119333, Russia
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64 citations as recorded by crossref.
- Historical and Projected Changes in the Southern Hemisphere Surface Westerlies R. Goyal et al. 10.1029/2020GL090849
- Seasonal Hydrodynamic Forecasts Using the INM-CM5 Model for Estimating the Beginning of Birch Pollen Dispersion S. Emelina et al. 10.1134/S0001433823040059
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- Overturning Pathways Control AMOC Weakening in CMIP6 Models J. Baker et al. 10.1029/2023GL103381
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- Projected Changes of Surface Winds Over the Antarctic Continental Margin J. Neme et al. 10.1029/2022GL098820
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- Analysis of the Atmosphere and the Ocean Upper Layer State Predictability for up to 5 Years Ahead Using the INMCM5 Climate Model Hindcasts V. Vorobeva et al. 10.3103/S106837392307004X
- Climatically Driven Minimum of Energy Demand for Heating in Cities at the Center of the European Part of Russia G. Alexandrov 10.1134/S000143382006002X
- Optimization of the Design of an Agrophotovoltaic System in Future Climate Conditions in South Korea S. Kim & S. Kim 10.2139/ssrn.4088352
- Reply to “Comment on ‘The Impact of Recent Forcing and Ocean Heat Uptake Data on Estimates of Climate Sensitivity’” N. Lewis & J. Curry 10.1175/JCLI-D-18-0669.1
- Hydrological Intensification Will Increase the Complexity of Water Resource Management D. Ficklin et al. 10.1029/2021EF002487
- Multi-model ensemble mean of global climate models fails to reproduce early twentieth century Arctic warming M. Latonin et al. 10.1016/j.polar.2021.100677
- Evaluation of the characteristics of Indian summer monsoon simulated by CMIP6 models M. Saha & C. Singh 10.1002/joc.8484
- Performance evaluation and ranking of CMIP6 global climate models over upper blue nile (abbay) basin of Ethiopia J. Mohammed 10.1016/j.nhres.2024.06.004
- Unusually low dust activity in North Africa in June 2023: Causes, impacts and future projections D. Francis et al. 10.1016/j.atmosres.2024.107594
- Climatological features of future MCSs over the Canadian Prairies using convection-permitting climate models Y. Hwang et al. 10.1016/j.atmosres.2023.106922
- Assessment of NEX-GDDP-CMIP6 Downscale Data in Simulating Extreme Precipitation over the Huai River Basin F. Jiang et al. 10.3390/atmos14101497
- Asymmetric effects of hydroclimate extremes on eastern US tree growth: Implications on current demographic shifts and climate variability J. Maxwell et al. 10.1111/gcb.17474
- Increasing Hurricane Intensification Rate Near the US Atlantic Coast K. Balaguru et al. 10.1029/2022GL099793
- Climatological features of future mesoscale convective systems in convection‐permitting climate models using CMIP6 and ERA5 in the central United States Y. Hwang et al. 10.1002/qj.4549
- Accuracy of historical precipitation from CMIP6 global climate models under diversified climatic features over India G. Patel et al. 10.1016/j.envdev.2024.100998
- Large-ensemble assessment of the Arctic stratospheric polar vortex morphology and disruptions A. Kuchar et al. 10.5194/wcd-5-895-2024
- Assessment of extreme rainfall events over the Indian subcontinent during the historical and future projection periods based on CMIP6 simulations P. Suthinkumar et al. 10.1002/joc.8314
- Future projections of seasonal temperature and precipitation for India P. Salunke et al. 10.3389/fclim.2023.1069994
- Simulation of Possible Future Climate Changes in the 21st Century in the INM-CM5 Climate Model E. Volodin & A. Gritsun 10.1134/S0001433820030123
- Comment on “The Impact of Recent Forcing and Ocean Heat Uptake Data on Estimates of Climate Sensitivity” K. Cowtan & P. Jacobs 10.1175/JCLI-D-18-0316.1
Discussed (final revised paper)
Latest update: 20 Nov 2024
Short summary
Climate changes of 1850–2014 are modeled with the climate model INM-CM5. Periods of fast warming in 1920–1940 and 1980–2000 as well as its slowdown in 1950–1975 and 2000–2014 are correctly reproduced by the model. The notable improvement with respect to the previous model version is the correct reproduction of slowdowns in global warming that we attribute to a new aerosol block in the model and a more accurate description of the solar constant in the new (CMIP6) IPCC protocol.
Climate changes of 1850–2014 are modeled with the climate model INM-CM5. Periods of fast warming...
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