A parameterization of sea‐salt aerosol source function for sub‐ and super‐micron particles

By S. Gong. 2003

669 citations recorded by the source corpus.

Subfields: Atmospheric Science, Global and Planetary Change

View Paper: https://www.semanticscholar.org/paper/5c99e61d97f6296e04140efcbf129de1dc6b6ac7

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Citations in the corpus

The AFWA dust emission scheme for the GOCART aerosol model in WRF-Chem v3.8.1 (2019, methodology): “Background sea salt emissions were based on the lowest model level wind speeds over the oceans (Gong, 2003), and the other background non-dust aerosol emissions within the domain were set using the PREP-CHEM-SRC preprocessing software (Freitas et al.”
The MERRA-2 Aerosol Reanalysis, 1980 - onward, Part I: System Description and Data Assimilation Evaluation. (2017, background): “The winddependent term in the Gong (2003) sea salt emission parameterization is updated to depend on friction velocity rather than 10-m velocity (i.e., u * , where u* is the friction velocity). We note that there are errant emissions of sea salt over the Great Lakes and Caspian and Black Seas due to”
Aerosol cloud precipitation interactions. Part 1. The nature and sources of cloud-active aerosols (2008, methodology): “They conclude that the best match with the observed size distributions (O'Dowd et al., 1997) is obtained using the Gong–Monahan and Vignati schemes (Vignati et al., 2001; Gong, 2003), among which the Gong–Monahan scheme probably has the more faithful representation of the wind-speed dependence.”
Using the OMI aerosol index and absorption aerosol optical depth to evaluate the NASA MERRA Aerosol Reanalysis (2014, methodology): “Production of sea-salt aerosols follows the Gong (2003) formulation of size-dependent number flux, but with a modified windspeed term equal to u2.”
Online simulations of global aerosol distributions in the NASA GEOS‐4 model and comparisons to satellite and ground‐based aerosol optical depth (2010, background): “, 1986], as modified by Gong [2003] to account better for the size distribution of small sea salt particles.”
The Modern-Era Retrospective Analysis for Research and Applications, Version 2 (MERRA-2). (2017, background): “Emissions of both dust and sea salt are wind-driven for each of ﬁve size bins, parameterized following Marticorena and Bergametti (1995) and Gong (2003), respectively.”
Impact of nucleation on global CCN (2009, methodology): “AEROCOM Sulfate AEROCOM AEROCOM AEROCOM Sea-salt Gong (2003) Martensson et al. (2003) Martensson et al. (2003) UTN H 2 SO 4 − H 2 O Kulmala et al. (1998) Kulmala et al. (1998) Vehkamäki et al. (2002) BLN Activation A=2x10 −7 A=2x10 −6 A=2x10 −5 processes include nucleation, primary particle emission”
Natural aerosol direct and indirect radiative effects (2013, background): “13 W m, which is substantially larger than that calculated by Goto et al. [2008] (–0.”
Importance of tropospheric volcanic aerosol for indirect radiative forcing of climate (2012, methodology): “Sea spray emissions are interactive in the model, driven by the wind speed at each timestep using the Gong (2003) size-resolved source function.”