A parameterization of aerosol activation: 2. Multiple aerosol types

By Hayder Abdul-Razzak, Steven Ghan. 2000

849 citations recorded by the source corpus.

Subfields: Atmospheric Science, Global and Planetary Change, Ocean Engineering

View Paper: https://www.semanticscholar.org/paper/9e360ce42016aad541eaad37db2b6299017605cc

How researchers see this paper

The researchers whose trusted networks rank it highest, strongest advocate first. Every researcher gets a different order.

In Atmospheric Science

1. Hugh Morrison
2. Andrew Gettelman
3. Xiaohong Liu
4. Steven Ghan
5. C. Hoose
6. Ulrike Lohmann
7. P. Stier
8. Minghuai Wang

In Global and Planetary Change

1. Hugh Morrison
2. Andrew Gettelman
3. Xiaohong Liu
4. Steven Ghan
5. C. Hoose
6. Ulrike Lohmann
7. P. Stier
8. J. Kristjánsson

In Ocean Engineering

1. Hugh Morrison
2. P. Stier
3. Andrew Gettelman
4. C. Hoose
5. A. Nenes
6. John H. Seinfeld
7. Xiaohong Liu
8. J. Kristjánsson

Citations in the corpus

• Detailed source term estimation of the atmospheric release for the Fukushima Daiichi Nuclear Power Station accident by coupling simulations of an atmospheric dispersion model with an improved deposition scheme and oceanic dispersion model (2014, methodology): “A4 Cloud condensation nuclei (CCN) activation For calculating fccn, the CCN activation and subsequent cloud microphysical processes were parameterized using Abdul-Razzak and Ghan (2000) and Lin et al. (1983). When the Abdul-Razzak and Ghan (2000) parameterization predicts that CCN activation occurs ”
• A New Parameterization of Cloud Droplet Activation Applicable to General Circulation Models (2006, methodology): “REFERENCES Abdul-Razzak, H., and S. J. Ghan, 2000: A parameterization of aerosol activation 2.”
• Global model simulations of the impact of ocean-going ships on aerosols, clouds, and the radiation budget (2007, methodology): “Aerosol activation is calculated following Abdul-Razzak and Ghan(2000).”
• Aerosol–climate interactions in the Norwegian Earth System Model – NorESM1-M (2012, methodology): “, 2009; see also Abdul-Razzak and Ghan, 2000). From a second set of look-up tables, spectrally resolved mass-specific extinction, single scattering albedo, and asymmetry factor are used to estimate the influence of aerosols on shortwave radiation. The maximum RH value in the look-up tables for these”
• An Overview of the Atmospheric Component of the Energy Exascale Earth System Model (2019, background): “Liquid cloud drop activation follows Abdul‐Razzak and Ghan (2000).”
• Improved Aerosol Processes and Effective Radiative Forcing in HadGEM3 and UKESM1 (2018, methodology): “While more advanced interactive aerosol activation parameterizations, like that of Abdul-Razzak and Ghan (2000), have significantly improved our ability to simulate global distributions of PD Nd (West et al., 2014), the response of Nd (and hence aerosol ERF) to aerosol changes over the historical…”
• Intercomparison and evaluation of global aerosol microphysical properties among AeroCom models of a range of complexity (2014, background): “…of these metrics are uniquely relevant to the aerosol effect on clouds and climate because the actual activation size depends on the particle chemical composition, cloud updraught velocity and the details of the full size distribution (e.g. Abdul-Razzak and Ghan, 2000; Nenes and Se-infeld, 2003).”
• Advanced Two-Moment Bulk Microphysics for Global Models. Part II: Global Model Solutions and Aerosol–Cloud Interactions* (2015, methodology): “(2012)) by droplet activation (Abdul-Razzak and Ghan 2000) and ice nucleation (Liu et al. 2007). CAM5.3 also has a separate moist turbulent boundary layer scheme (Bretherton and Park 2009), a shallow convective parameterization (Park and Bretherton 2009), and a deep convective scheme (Zhang and McFa”
• Global indirect aerosol effects: a review (2004, neutral): “While the effect of surface active organics has recently been included in the parameterization of cloud droplet formation byAbdul-Razzak and Ghan (2004), other effects of organics, such as their film-forming ability are not considered yet.”
• A numerical study of the effect of different aerosol types on East Asian summer clouds and precipitation (2013, neutral): “The aerosol effect on stratiform cloud microphysics through droplet activation is parameterized in terms of sub-grid cloud scale vertical velocity, and size distribution and volume-mean hygroscopicity of aerosol modes (Abdul-Razzak and Ghan, 2000).”
• Constraining cloud droplet number concentration in GCMs suppresses the aerosol indirect effect (2009, methodology): “The activation of aerosol particles into cloud droplets is calculated at all cloudy gridpoints as a function of aerosol composition and the subgrid-scale updraft velocity [Abdul-Razzak and Ghan, 2000].”