Articles | Volume 16, issue 23
https://doi.org/10.5194/acp-16-15413-2016
© Author(s) 2016. This work is distributed under
the Creative Commons Attribution 3.0 License.
the Creative Commons Attribution 3.0 License.
https://doi.org/10.5194/acp-16-15413-2016
© Author(s) 2016. This work is distributed under
the Creative Commons Attribution 3.0 License.
the Creative Commons Attribution 3.0 License.
The source of discrepancies in aerosol–cloud–precipitation interactions between GCM and A-Train retrievals
Takuro Michibata
CORRESPONDING AUTHOR
Department of Earth System Science and Technology, Kyushu University, Fukuoka, Japan
Research Institute for Applied Mechanics, Kyushu University, Fukuoka, Japan
Kentaroh Suzuki
Atmosphere and Ocean Research Institute, The University of Tokyo, Chiba, Japan
Yousuke Sato
RIKEN Advanced Institute for Computational Science, Hyogo, Japan
Toshihiko Takemura
Research Institute for Applied Mechanics, Kyushu University, Fukuoka, Japan
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- Simulation of the responses of rainstorm in the Yangtze River Middle Reaches to changes in anthropogenic aerosol emissions Y. Bai et al. 10.1016/j.atmosenv.2019.117081
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- Response of the atmospheric hydrological cycle over the tropical Asian monsoon regions to anthropogenic aerosols and its seasonality H. Takahashi et al. 10.1186/s40645-018-0197-2
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- Deconvolution of boundary layer depth and aerosol constraints on cloud water path in subtropical stratocumulus decks A. Possner et al. 10.5194/acp-20-3609-2020
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- Aerosol-driven droplet concentrations dominate coverage and water of oceanic low-level clouds D. Rosenfeld et al. 10.1126/science.aav0566
- Aerosol effects on clouds are concealed by natural cloud heterogeneity and satellite retrieval errors A. Arola et al. 10.1038/s41467-022-34948-5
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- Interpretation of Aerosol Effects on Precipitation Susceptibility in Warm Clouds Inferred from Satellite Measurements and Model Evaluation over Northeast Asia S. Park & C. Kim 10.1175/JAS-D-20-0293.1
- Cloud Top Radiative Cooling Rate Drives Non‐Precipitating Stratiform Cloud Responses to Aerosol Concentration A. Williams & A. Igel 10.1029/2021GL094740
- Connecting regional aerosol emissions reductions to local and remote precipitation responses D. Westervelt et al. 10.5194/acp-18-12461-2018
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- Too Frequent and Too Light Arctic Snowfall With Incorrect Precipitation Phase Partitioning in the MIROC6 GCM Y. Imura & T. Michibata 10.1029/2022MS003046
- Assessing the impact of the Kuroshio Current on vertical cloud structure using CloudSat data A. Yamauchi et al. 10.5194/acp-18-7657-2018
- A development of reduction scenarios of the short-lived climate pollutants (SLCPs) for mitigating global warming and environmental problems T. Nakajima et al. 10.1186/s40645-020-00351-1
- Bounding Global Aerosol Radiative Forcing of Climate Change N. Bellouin et al. 10.1029/2019RG000660
- Prognostic Precipitation in the MIROC6‐SPRINTARS GCM: Description and Evaluation Against Satellite Observations T. Michibata et al. 10.1029/2018MS001596
- Strengthened Indian Summer Monsoon Precipitation Susceptibility Linked to Dust‐Induced Ice Cloud Modification P. Patel et al. 10.1029/2018GL081634
- A Multimodel Study on Warm Precipitation Biases in Global Models Compared to Satellite Observations X. Jing et al. 10.1002/2017JD027310
- The Key Role of Warm Rain Parameterization in Determining the Aerosol Indirect Effect in a Global Climate Model X. Jing et al. 10.1175/JCLI-D-18-0789.1
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- Aerosol-cloud-climate cooling overestimated by ship-track data F. Glassmeier et al. 10.1126/science.abd3980
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- Machine-Learning Based Analysis of Liquid Water Path Adjustments to Aerosol Perturbations in Marine Boundary Layer Clouds Using Satellite Observations L. Zipfel et al. 10.3390/atmos13040586
- Constraining the Twomey effect from satellite observations: issues and perspectives J. Quaas et al. 10.5194/acp-20-15079-2020
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Discussed (final revised paper)
Latest update: 14 Dec 2024
Short summary
This study identifies a fundamental flaw of a GCM in aerosol–cloud–precipitation interactions. The model predicts a monotonic increase in the LWP in response to increased aerosols, which is in stark contrast to satellite retrievals that show a regional variation in the sign of the LWP response. The model also fails to represent the observed dependency of the LWP response on macrophysical regimes. The model biases are attributed to the autoconversion process, with a lack of buffering mechanisms.
This study identifies a fundamental flaw of a GCM in aerosol–cloud–precipitation...
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