Articles | Volume 14, issue 21
https://doi.org/10.5194/acp-14-11997-2014
© Author(s) 2014. 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-14-11997-2014
© Author(s) 2014. This work is distributed under
the Creative Commons Attribution 3.0 License.
the Creative Commons Attribution 3.0 License.
Impact of the representation of marine stratocumulus clouds on the anthropogenic aerosol effect
ETH Zurich, Institute for Atmospheric and Climate Science, Zurich, Switzerland
U. Lohmann
ETH Zurich, Institute for Atmospheric and Climate Science, Zurich, Switzerland
Karlsruhe Institute of Technology, Institute for Meteorology and Climate Research, Karlsruhe, Germany
M. G. Frontoso
ETH Zurich, Institute for Atmospheric and Climate Science, Zurich, Switzerland
ETH Zurich, Center for Climate System Modeling, Zurich, Switzerland
now at: RMS, Zurich, Switzerland
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46 citations as recorded by crossref.
- On the characteristics of aerosol indirect effect based on dynamic regimes in global climate models S. Zhang et al. 10.5194/acp-16-2765-2016
- Influence of horizontal resolution and complexity of aerosol–cloud interactions on marine stratocumulus and stratocumulus‐to‐cumulus transition in HadGEM3‐GC3.1 A. Ekman et al. 10.1002/qj.4494
- Effect of anthropogenic aerosol emissions on precipitation in warm conveyor belts in the western North Pacific in winter – a model study with ECHAM6-HAM H. Joos et al. 10.5194/acp-17-6243-2017
- The importance of mixed-phase and ice clouds for climate sensitivity in the global aerosol–climate model ECHAM6-HAM2 U. Lohmann & D. Neubauer 10.5194/acp-18-8807-2018
- Aerosol and physical atmosphere model parameters are both important sources of uncertainty in aerosol ERF L. Regayre et al. 10.5194/acp-18-9975-2018
- Bounding Global Aerosol Radiative Forcing of Climate Change N. Bellouin et al. 10.1029/2019RG000660
- The global aerosol–climate model ECHAM6.3–HAM2.3 – Part 2: Cloud evaluation, aerosol radiative forcing, and climate sensitivity D. Neubauer et al. 10.5194/gmd-12-3609-2019
- Spatial Aggregation of Satellite Observations Leads to an Overestimation of the Radiative Forcing due to Aerosol‐Cloud Interactions T. Goren et al. 10.1029/2023GL105282
- Additional global climate cooling by clouds due to ice crystal complexity E. Järvinen et al. 10.5194/acp-18-15767-2018
- Vertical grid refinement for stratocumulus clouds in the radiation scheme of the global climate model ECHAM6.3-HAM2.3-P3 P. Pelucchi et al. 10.5194/gmd-14-5413-2021
- Unanticipated Side Effects of Stratospheric Albedo Modification Proposals Due to Aerosol Composition and Phase D. Cziczo et al. 10.1038/s41598-019-53595-3
- Does prognostic seeding along flight tracks produce the desired effects of cirrus cloud thinning? C. Tully et al. 10.5194/acp-23-7673-2023
- Tropospheric warming over the northern Indian Ocean caused by South Asian anthropogenic aerosols: possible impact on the upper troposphere and lower stratosphere S. Fadnavis et al. 10.5194/acp-22-7179-2022
- An underestimated negative cloud feedback from cloud lifetime changes J. Mülmenstädt et al. 10.1038/s41558-021-01038-1
- Cirrus cloud thinning using a more physically based ice microphysics scheme in the ECHAM-HAM general circulation model C. Tully et al. 10.5194/acp-22-11455-2022
- Potential impact of carbonaceous aerosol on the upper troposphere and lower stratosphere (UTLS) and precipitation during Asian summer monsoon in a global model simulation S. Fadnavis et al. 10.5194/acp-17-11637-2017
- Impacts on cloud radiative effects induced by coexisting aerosols converted from international shipping and maritime DMS emissions Q. Jin et al. 10.5194/acp-18-16793-2018
- Investigating the impact of haze on MODIS cloud detection F. Mao et al. 10.1002/2015JD023555
- Unveiling aerosol–cloud interactions – Part 2: Minimising the effects of aerosol swelling and wet scavenging in ECHAM6-HAM2 for comparison to satellite data D. Neubauer et al. 10.5194/acp-17-13165-2017
- Reducing the aerosol forcing uncertainty using observational constraints on warm rain processes J. Mülmenstädt et al. 10.1126/sciadv.aaz6433
- Immersion mode ice nucleation measurements with the new Portable Immersion Mode Cooling chAmber (PIMCA) M. Kohn et al. 10.1002/2016JD024761
- Is increasing ice crystal sedimentation velocity in geoengineering simulations a good proxy for cirrus cloud seeding? B. Gasparini et al. 10.5194/acp-17-4871-2017
- The chemistry–climate model ECHAM6.3-HAM2.3-MOZ1.0 M. Schultz et al. 10.5194/gmd-11-1695-2018
- Cirrus Cloud Properties as Seen by the CALIPSO Satellite and ECHAM-HAM Global Climate Model B. Gasparini et al. 10.1175/JCLI-D-16-0608.1
- Anthropogenic Air Pollution Delays Marine Stratocumulus Breakup to Open Cells T. Goren et al. 10.1029/2019GL085412
- Amplified drying in South Asian summer monsoon precipitation due to anthropogenic sulfate aerosols S. Fadnavis et al. 10.1016/j.envpol.2023.123175
- Impact of Resolution on the Representation of Precipitation Variability Associated With the ITCZ M. De Benedetti & G. Moore 10.1002/2017GL075714
- The impact of recent changes in Asian anthropogenic emissions of SO<sub>2</sub> on sulfate loading in the upper troposphere and lower stratosphere and the associated radiative changes S. Fadnavis et al. 10.5194/acp-19-9989-2019
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- Strong impacts on aerosol indirect effects from historical oxidant changes I. Karset et al. 10.5194/acp-18-7669-2018
- Elucidating ice formation pathways in the aerosol–climate model ECHAM6-HAM2 R. Dietlicher et al. 10.5194/acp-19-9061-2019
- Measurement report: Cloud processes and the transport of biological emissions affect southern ocean particle and cloud condensation nuclei concentrations K. Sanchez et al. 10.5194/acp-21-3427-2021
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- Implementing microscopic charcoal particles into a global aerosol–climate model A. Gilgen et al. 10.5194/acp-18-11813-2018
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- Decomposing the effective radiative forcing of anthropogenic aerosols based on CMIP6 Earth system models A. Kalisoras et al. 10.5194/acp-24-7837-2024
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Latest update: 21 Nov 2024
Short summary
Several biases in the representation of clouds in the stratocumulus regime in the ECHAM6-HAM2 global climate model were found by evaluating the model in the stratocumulus cloud regime. Simulations with changes in model resolution and physics to better represent clouds and aerosol in the stratocumulus regime show that the human influence on clouds and thus climate by emission of aerosol particles is sensitive to the representation of (stratocumulus) clouds.
Several biases in the representation of clouds in the stratocumulus regime in the ECHAM6-HAM2...
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