Articles | Volume 16, issue 10
https://doi.org/10.5194/acp-16-6595-2016
© 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-16-6595-2016
© Author(s) 2016. This work is distributed under
the Creative Commons Attribution 3.0 License.
the Creative Commons Attribution 3.0 License.
Limitations of passive remote sensing to constrain global cloud condensation nuclei
Philip Stier
CORRESPONDING AUTHOR
Atmospheric, Oceanic and Planetary Physics, Department of Physics,
University of Oxford, Oxford, UK
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- The Global Atmosphere‐aerosol Model ICON‐A‐HAM2.3–Initial Model Evaluation and Effects of Radiation Balance Tuning on Aerosol Optical Thickness M. Salzmann et al. 10.1029/2021MS002699
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- Constraining effects of aerosol-cloud interaction by accounting for coupling between cloud and land surface T. Su et al. 10.1126/sciadv.adl5044
- Significant underestimation of radiative forcing by aerosol–cloud interactions derived from satellite-based methods H. Jia et al. 10.1038/s41467-021-23888-1
- A machine learning paradigm for necessary observations to reduce uncertainties in aerosol climate forcing J. Redemann & L. Gao 10.1038/s41467-024-52747-y
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- Reducing uncertainties in satellite estimates of aerosol–cloud interactions over the subtropical ocean by integrating vertically resolved aerosol observations D. Painemal et al. 10.5194/acp-20-7167-2020
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- Passive remote sensing of aerosol layer height using near‐UV multiangle polarization measurements L. Wu et al. 10.1002/2016GL069848
- Sensitivity of cloud microphysics to aerosol is highly associated with cloud water content: Implications for indirect radiative forcing Y. Wang et al. 10.1016/j.atmosres.2024.107552
- Cloud water adjustments to aerosol perturbations are buffered by solar heating in non-precipitating marine stratocumuli J. Zhang et al. 10.5194/acp-24-10425-2024
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- Spatial Heterogeneity of Aerosol Effect on Liquid Cloud Microphysical Properties in the Warm Season Over Tibetan Plateau P. Zhao et al. 10.1029/2022JD037738
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- Observational constraint on cloud susceptibility weakened by aerosol retrieval limitations P. Ma et al. 10.1038/s41467-018-05028-4
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- Nonlinearity of the cloud response postpones climate penalty of mitigating air pollution in polluted regions H. Jia & J. Quaas 10.1038/s41558-023-01775-5
- Relationship between cloud condensation nuclei (CCN) concentration and aerosol optical depth in the Arctic region S. Ahn et al. 10.1016/j.atmosenv.2021.118748
- Reducing Aerosol Forcing Uncertainty by Combining Models With Satellite and Within‐The‐Atmosphere Observations: A Three‐Way Street R. Kahn et al. 10.1029/2022RG000796
- Development of ZJU high-spectral-resolution lidar for aerosol and cloud: Feature detection and classification N. Wang et al. 10.1016/j.jqsrt.2021.107513
- Observing short-timescale cloud development to constrain aerosol–cloud interactions E. Gryspeerdt et al. 10.5194/acp-22-11727-2022
- A Case Study in Low Aerosol Number Concentrations Over the Eastern North Atlantic: Implications for Pristine Conditions in the Remote Marine Boundary Layer S. Pennypacker & R. Wood 10.1002/2017JD027493
- Opposite Aerosol Index‐Cloud Droplet Effective Radius Correlations Over Major Industrial Regions and Their Adjacent Oceans X. Ma et al. 10.1029/2018GL077562
- Validation of satellite-retrieved CCN based on a cruise campaign over the polluted Northwestern Pacific ocean Y. Wang et al. 10.1016/j.atmosres.2021.105722
- Spaceborne Lidar in the Study of Marine Systems C. Hostetler et al. 10.1146/annurev-marine-121916-063335
- Frontiers in Satellite‐Based Estimates of Cloud‐Mediated Aerosol Forcing D. Rosenfeld et al. 10.1029/2022RG000799
- The importance of comprehensive parameter sampling and multiple observations for robust constraint of aerosol radiative forcing J. Johnson et al. 10.5194/acp-18-13031-2018
- Effects of auxiliary atmospheric state parameters on the aerosol optical properties retrieval errors of high-spectral-resolution lidar Y. Zhang et al. 10.1364/AO.57.002627
- Estimating cloud condensation nuclei concentrations from CALIPSO lidar measurements G. Choudhury & M. Tesche 10.5194/amt-15-639-2022
- Impact of Saharan dust on North Atlantic marine stratocumulus clouds: importance of the semidirect effect A. Amiri-Farahani et al. 10.5194/acp-17-6305-2017
- Cloud drop number concentrations over the western North Atlantic Ocean: seasonal cycle, aerosol interrelationships, and other influential factors H. Dadashazar et al. 10.5194/acp-21-10499-2021
- Machine Learning Approach to Investigating the Relative Importance of Meteorological and Aerosol-Related Parameters in Determining Cloud Microphysical Properties F. Bender et al. 10.16993/tellusb.1868
- Potential Modulation of Aerosol on Precipitation Efficiency in Southwest China P. Zhao et al. 10.3390/rs16081445
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Discussed (final revised paper)
Latest update: 23 Nov 2024
Short summary
Cloud droplets form on suitable nuclei from aerosol emissions. Clouds with more droplets have higher reflectance so that aerosol emissions have a cooling climate effect. Numerous publications of these effects rely on passive satellite remote sensing. In this work I use a self consistent global aerosol model to show that a commonly used assumption (passively retrieved aerosol extinction is a suitable proxy for cloud condensation nuclei) is violated for a significant fraction of the Earth.
Cloud droplets form on suitable nuclei from aerosol emissions. Clouds with more droplets have...
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