Biogenically driven organic contribution to marine aerosol
By C. O’Dowd, M. Facchini, F. Cavalli, D. Ceburnis, M. Mircea, S. Decesari, S. Fuzzi, Y. Yoon, J. Putaud. Nature, 2004
992 citations recorded by the source corpus.
Subfields: Atmospheric Science, Global and Planetary Change
View Paper: https://www.semanticscholar.org/paper/89dda58da3be90411a98aaf20b113450b713146d
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Citations in the corpus
- Aerosol cloud precipitation interactions. Part 1. The nature and sources of cloud-active aerosols (2008, background): “The fraction of organic components increases with decreasing particle size, and, in biologically active regions, may approach 90% in the size fraction around 100 nm (Cavalli et al., 2004; O'Dowd et al., 2004; Keene et al., 2007; Nilsson et al., 2007).”
- Ambient nano and ultrafine particles from motor vehicle emissions: Characteristics, ambient processing and implications on human exposure (2008, background): “…upon which vapours can condense (Kulmala et al. 2000), free tropospheric production with mixing down to the boundary layer (Raes 1995), and the generation of coastal iodine particles from macroalgal iodocarbon emissions (Raes 1995; Kulmala et al. 2000; O'Dowd et al. 2004; O'Dowd and Hoffmann 2005).”
- Global indirect aerosol effects: a review (2004, neutral): “Other GCMs avoid this issue completely and use empirical relationships between aerosol mass and cloud droplet number concentration instead (Menon et al., 2002a).”
- Improved Aerosol Processes and Effective Radiative Forcing in HadGEM3 and UKESM1 (2018, background): “Recent studies also highlight the additional large contribution of biogenic aerosol from marine organic sources to the CCN population in pristine marine regions in both NH and SH (Meskhidze & Nenes, 2006; O’Dowd et al., 2004).”
- Marine aerosol production: a review of the current knowledge (2007, background): “Figure 5 illustrates the chemical composition of clean marine aerosol over the northeast Atlantic during winter and summer periods, corresponding to low and high biological activity periods (O’Dowd et al. 2004).”
- Aerosol–climate interactions in the Norwegian Earth System Model – NorESM1-M (2012, background): “These emissions depend on 10-m wind speed (U10) and sea surface temperature (SST) (M̊artensson et al., 2003), and are regulated by the sea ice cover as in Nilsson et al. (2001).”