Articles | Volume 12, issue 7
https://doi.org/10.5194/gmd-12-2875-2019
© Author(s) 2019. This work is distributed under
the Creative Commons Attribution 4.0 License.
the Creative Commons Attribution 4.0 License.
https://doi.org/10.5194/gmd-12-2875-2019
© Author(s) 2019. This work is distributed under
the Creative Commons Attribution 4.0 License.
the Creative Commons Attribution 4.0 License.
Development and technical paper
| 
12 Jul 2019
Development and technical paper |
| 12 Jul 2019
| 12 Jul 2019
Significant improvement of cloud representation in the global climate model MRI-ESM2
Meteorological Research Institute, Japan Meteorological Agency,
Tsukuba, 305-0052, Japan
Seiji Yukimoto
Meteorological Research Institute, Japan Meteorological Agency,
Tsukuba, 305-0052, Japan
Tsuyoshi Koshiro
Meteorological Research Institute, Japan Meteorological Agency,
Tsukuba, 305-0052, Japan
Naga Oshima
Meteorological Research Institute, Japan Meteorological Agency,
Tsukuba, 305-0052, Japan
Taichu Tanaka
Meteorological Research Institute, Japan Meteorological Agency,
Tsukuba, 305-0052, Japan
Hiromasa Yoshimura
Meteorological Research Institute, Japan Meteorological Agency,
Tsukuba, 305-0052, Japan
Ryoji Nagasawa
Meteorological Research Institute, Japan Meteorological Agency,
Tsukuba, 305-0052, Japan
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73 citations as recorded by crossref.
- An Overview of the Extratropical Storm Tracks in CMIP6 Historical Simulations M. Priestley et al. 10.1175/JCLI-D-19-0928.1
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- An evaluation of the Arctic clouds and surface radiative fluxes in CMIP6 models J. Wei et al. 10.1007/s13131-021-1705-6
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- Improved Representation of Low‐Level Mixed‐Phase Clouds in a Global Cloud‐System‐Resolving Simulation A. Noda et al. 10.1029/2021JD035223
- On the Effect of Historical SST Patterns on Radiative Feedback T. Andrews et al. 10.1029/2022JD036675
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- SimCloud version 1.0: a simple diagnostic cloud scheme for idealized climate models Q. Liu et al. 10.5194/gmd-14-2801-2021
- Changes in Dust Emissions in the Gobi Desert due to Global Warming Using MRI-ESM2.0 T. Maki et al. 10.2151/sola.2022-035
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- Evaluation of Past and Future Climate Trends under CMIP6 Scenarios for the UBNB (Abay), Ethiopia A. Alaminie et al. 10.3390/w13152110
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- RANGE DYNAMICS OF POTATO NEMATODE <i>GLOBODERA ROSTOCHIENSIS</i> (WOLLENWEBER, 1923) SKARBILOVICH, 1959 UNDER CONDITIONS OF GLOBAL CLIMATE CHANGE IN RUSSIA M. Pridannikov et al. 10.35885/1996-1499-15-3-135-159
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- CMIP6 projected trend of winter and summer variation in Arctic cyclones over the 21st century J. Song et al. 10.1007/s00382-024-07531-5
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- Tropospheric cooling induces annual wet biases over China in CMIP6 models L. Wang et al. 10.1007/s00382-024-07410-z
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- Role of Interhemispheric Heat Transport and Global Atmospheric Cooling in Multidecadal Trends of Northern Hemisphere Precipitation S. Yukimoto et al. 10.1029/2022GL100335
- Evaluation of the CMIP6 marine subtropical stratocumulus cloud albedo and its controlling factors B. Jian et al. 10.5194/acp-21-9809-2021
- Model evaluation of short-lived climate forcers for the Arctic Monitoring and Assessment Programme: a multi-species, multi-model study C. Whaley et al. 10.5194/acp-22-5775-2022
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- Evaluation of CMIP6 GCM rainfall in mainland Southeast Asia Z. Iqbal et al. 10.1016/j.atmosres.2021.105525
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- Range Dynamics of Striped Field Mouse (Apodemus agrarius) in Northern Eurasia under Global Climate Change Based on Ensemble Species Distribution Models V. Petrosyan et al. 10.3390/biology12071034
- Evaluation and correction analysis of the regional rainfall simulation by CMIP6 over Sudan W. Babiker et al. 10.5937/gp28-46565
- Global and Arctic effective radiative forcing of anthropogenic gases and aerosols in MRI-ESM2.0 N. Oshima et al. 10.1186/s40645-020-00348-w
- Improvements in Supercooled Liquid Water Simulations of Low-Level Mixed-Phase Clouds over the Southern Ocean Using a Single-Column Model T. Seiki & W. Roh 10.1175/JAS-D-19-0266.1
- How do CMIP6 models project changes in precipitation extremes over seasons and locations across the mid hills of Nepal? R. Chhetri et al. 10.1007/s00704-021-03698-7
- On the emergence of a predicted climate change signal: When and where it could appear over Pakistan B. Khan et al. 10.29333/ejosdr/12561
- Marine aerosol feedback on biogeochemical cycles and the climate in the Anthropocene: lessons learned from the Pacific Ocean A. Ito et al. 10.1039/D2EA00156J
- Next-Generation Drought Intensity–Duration–Frequency Curves for Early Warning Systems in Ethiopia’s Pastoral Region G. Tegegne et al. 10.3390/cli13020031
- Assessment of the capability of CMIP6 global climate models to simulate Arctic cyclones J. Song et al. 10.1016/j.accre.2021.07.007
- Relationship between shortwave radiation bias over the Southern Ocean and the double‐intertropical convergence zone problem in MRI‐ESM2 H. Kawai et al. 10.1002/asl.1064
- Statistical characteristics of extreme daily precipitation during 1501 BCE–1849 CE in the Community Earth System Model W. Kim et al. 10.5194/cp-17-2031-2021
- Low‐Level Marine Tropical Clouds in Six CMIP6 Models Are Too Few, Too Bright but Also Too Compact and Too Homogeneous D. Konsta et al. 10.1029/2021GL097593
- Utilizing machine learning and CMIP6 projections for short-term agricultural drought monitoring in central Europe (1900–2100) S. Mohammed et al. 10.1016/j.jhydrol.2024.130968
Latest update: 23 Apr 2025
Short summary
The representation of clouds was significantly improved in the climate model MRI-ESM2. The model is planned for use in the sixth phase of the Coupled Model Intercomparison Project (CMIP6) simulations. In particular, a notorious lack of reflection of solar radiation over the Southern Ocean was drastically improved in the model. The score of the spatial pattern of radiative fluxes for MRI-ESM2 is better than for any CMIP5 model. We present modifications implemented in the various physics schemes.
The representation of clouds was significantly improved in the climate model MRI-ESM2. The model...
