Articles | Volume 19, issue 8
Atmos. Chem. Phys., 19, 5331–5347, 2019
https://doi.org/10.5194/acp-19-5331-2019
© Author(s) 2019. This work is distributed under
the Creative Commons Attribution 4.0 License.
the Creative Commons Attribution 4.0 License.
Atmos. Chem. Phys., 19, 5331–5347, 2019
https://doi.org/10.5194/acp-19-5331-2019
© Author(s) 2019. This work is distributed under
the Creative Commons Attribution 4.0 License.
the Creative Commons Attribution 4.0 License.
Research article 18 Apr 2019
Research article | 18 Apr 2019
Constraining the aerosol influence on cloud liquid water path
Edward Gryspeerdt et al.
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Cited
43 citations as recorded by crossref.
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- Simulation of Aerosol Indirect Effects on Cloud Streets Over the Northwestern Pacific Ocean C. Wu & J. Chen 10.1029/2020JD034325
- Exploring Impacts of Size‐Dependent Evaporation and Entrainment in a Global Model I. Karset et al. 10.1029/2019JD031817
- Anthropogenic emissions from South Asia reverses the aerosol indirect effect over the northern Indian Ocean S. Jose et al. 10.1038/s41598-020-74897-x
- A new classification of satellite-derived liquid water cloud regimes at cloud scale C. Unglaub et al. 10.5194/acp-20-2407-2020
- The Impact of Resolving Subkilometer Processes on Aerosol‐Cloud Interactions of Low‐Level Clouds in Global Model Simulations C. Terai et al. 10.1029/2020MS002274
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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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- Radiative forcing of the aerosol-cloud interaction in seriously polluted East China and East China Sea X. Zhang et al. 10.1016/j.atmosres.2020.105405
- Bounding Global Aerosol Radiative Forcing of Climate Change N. Bellouin et al. 10.1029/2019RG000660
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43 citations as recorded by crossref.
- Cloud Top Radiative Cooling Rate Drives Non‐Precipitating Stratiform Cloud Responses to Aerosol Concentration A. Williams & A. Igel 10.1029/2021GL094740
- Simulation of Aerosol Indirect Effects on Cloud Streets Over the Northwestern Pacific Ocean C. Wu & J. Chen 10.1029/2020JD034325
- Exploring Impacts of Size‐Dependent Evaporation and Entrainment in a Global Model I. Karset et al. 10.1029/2019JD031817
- Anthropogenic emissions from South Asia reverses the aerosol indirect effect over the northern Indian Ocean S. Jose et al. 10.1038/s41598-020-74897-x
- A new classification of satellite-derived liquid water cloud regimes at cloud scale C. Unglaub et al. 10.5194/acp-20-2407-2020
- The Impact of Resolving Subkilometer Processes on Aerosol‐Cloud Interactions of Low‐Level Clouds in Global Model Simulations C. Terai et al. 10.1029/2020MS002274
- Atmospheric energy budget response to idealized aerosol perturbation in tropical cloud systems G. Dagan et al. 10.5194/acp-20-4523-2020
- Aerosol-cloud-climate cooling overestimated by ship-track data F. Glassmeier et al. 10.1126/science.abd3980
- Quantifying variations in shortwave aerosol–cloud–radiation interactions using local meteorology and cloud state constraints A. Douglas & T. L'Ecuyer 10.5194/acp-19-6251-2019
- Surprising similarities in model and observational aerosol radiative forcing estimates E. Gryspeerdt et al. 10.5194/acp-20-613-2020
- Identifying Particle Growth Processes in Marine Low Clouds Using Spatial Variances of Imager‐Derived Cloud Parameters T. Nagao & K. Suzuki 10.1029/2020GL087121
- Substantial Cloud Brightening From Shipping in Subtropical Low Clouds M. Diamond et al. 10.1029/2019AV000111
- Observing the timescales of aerosol–cloud interactions in snapshot satellite images E. Gryspeerdt et al. 10.5194/acp-21-6093-2021
- Snow-induced buffering in aerosol–cloud interactions T. Michibata et al. 10.5194/acp-20-13771-2020
- 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
- Reducing the aerosol forcing uncertainty using observational constraints on warm rain processes J. Mülmenstädt et al. 10.1126/sciadv.aaz6433
- Quantifying cloud adjustments and the radiative forcing due to aerosol–cloud interactions in satellite observations of warm marine clouds A. Douglas & T. L'Ecuyer 10.5194/acp-20-6225-2020
- Radiative forcing of the aerosol-cloud interaction in seriously polluted East China and East China Sea X. Zhang et al. 10.1016/j.atmosres.2020.105405
- Bounding Global Aerosol Radiative Forcing of Climate Change N. Bellouin et al. 10.1029/2019RG000660
- Southern Ocean Cloud Properties Derived From CAPRICORN and MARCUS Data G. Mace et al. 10.1029/2020JD033368
- Radiative forcing of climate change from the Copernicus reanalysis of atmospheric composition N. Bellouin et al. 10.5194/essd-12-1649-2020
- Detection and attribution of aerosol–cloud interactions in large-domain large-eddy simulations with the ICOsahedral Non-hydrostatic model M. Costa-Surós et al. 10.5194/acp-20-5657-2020
- Modulated Responses of East Asian Winter Climate to Anthropogenic Aerosols by Urban Cover in Eastern China J. Deng et al. 10.3390/atmos12040471
- A First Case Study of CCN Concentrations from Spaceborne Lidar Observations A. Georgoulias et al. 10.3390/rs12101557
- Weak average liquid-cloud-water response to anthropogenic aerosols V. Toll et al. 10.1038/s41586-019-1423-9
- The Fall and Rise of the Global Climate Model J. Mülmenstädt & L. Wilcox 10.1029/2021MS002781
- Weak sensitivity of cloud water to aerosols A. Possner 10.1038/d41586-019-02287-z
- Future warming exacerbated by aged-soot effect on cloud formation U. Lohmann et al. 10.1038/s41561-020-0631-0
- The hemispheric contrast in cloud microphysical properties constrains aerosol forcing I. McCoy et al. 10.1073/pnas.1922502117
- Evaluation of the CMIP6 marine subtropical stratocumulus cloud albedo and its controlling factors B. Jian et al. 10.5194/acp-21-9809-2021
- Ensemble daily simulations for elucidating cloud–aerosol interactions under a large spread of realistic environmental conditions G. Dagan & P. Stier 10.5194/acp-20-6291-2020
- The Impact of Ship Emission Controls Recorded by Cloud Properties E. Gryspeerdt et al. 10.1029/2019GL084700
- Reconciling Compensating Errors Between Precipitation Constraints and the Energy Budget in a Climate Model T. Michibata & K. Suzuki 10.1029/2020GL088340
- Liquid Containing Clouds at the North Slope of Alaska Demonstrate Sensitivity to Local Industrial Aerosol Emissions M. Maahn et al. 10.1029/2021GL094307
- Present and future aerosol impacts on Arctic climate change in the GISS-E2.1 Earth system model U. Im et al. 10.5194/acp-21-10413-2021
- Separating radiative forcing by aerosol–cloud interactions and rapid cloud adjustments in the ECHAM–HAMMOZ aerosol–climate model using the method of partial radiative perturbations J. Mülmenstädt et al. 10.5194/acp-19-15415-2019
- Untangling causality in midlatitude aerosol–cloud adjustments D. McCoy et al. 10.5194/acp-20-4085-2020
- Constraining the Twomey effect from satellite observations: issues and perspectives J. Quaas et al. 10.5194/acp-20-15079-2020
- Trends in AOD, Clouds, and Cloud Radiative Effects in Satellite Data and CMIP5 and CMIP6 Model Simulations Over Aerosol Source Regions R. Cherian & J. Quaas 10.1029/2020GL087132
- Quantification of the Radiative Effect of Aerosol–Cloud Interactions in Shallow Continental Cumulus Clouds I. Glenn et al. 10.1175/JAS-D-19-0269.1
- Large‐Scale Industrial Cloud Perturbations Confirm Bidirectional Cloud Water Responses to Anthropogenic Aerosols H. Trofimov et al. 10.1029/2020JD032575
- Modelling the relationship between liquid water content and cloud droplet number concentration observed in low clouds in the summer Arctic and its radiative effects J. Dionne et al. 10.5194/acp-20-29-2020
- Cloud Microphysical Implications for Marine Cloud Brightening: The Importance of the Seeded Particle Size Distribution F. Hoffmann & G. Feingold 10.1175/JAS-D-21-0077.1
Latest update: 23 Sep 2021
Short summary
The liquid water path (LWP) is the strongest control on cloud albedo, such that a small change in LWP can have a large radiative impact. By changing the droplet number concentration (Nd) aerosols may be able to change the LWP, but the sign and magnitude of the effect is unclear. This work uses satellite data to investigate the relationship between Nd and LWP at a global scale and in response to large aerosol perturbations, suggesting that a strong decrease in LWP at high Nd may be overestimated.
The liquid water path (LWP) is the strongest control on cloud albedo, such that a small change...
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