Angstrom exponent and bimodal aerosol size distributions
By Gregory L. Schuster, Oleg Dubovik, Brent N. Holben. 2006
824 citations recorded by the source corpus.
Subfields: Atmospheric Science, Global and Planetary Change
View Paper: https://www.semanticscholar.org/paper/25bba2b0553f066eed08bf1096dc2a4f3acec131
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
- Brent N. Holben
- Oleg Dubovik
- Thomas F. Eck
- Alexander Sinyuk
- Yoram J. Kaufman
- Ping Yang
- Ilya Slutsker
- M. I. Mishchenko
In Global and Planetary Change
- Brent N. Holben
- Oleg Dubovik
- Thomas F. Eck
- Alexander Sinyuk
- Yoram J. Kaufman
- Ping Yang
- Ilya Slutsker
- M. I. Mishchenko
Citations in the corpus
- Classification of aerosol properties derived from AERONET direct sun data (2006, background): “Unsupervised classification of aerosol using numerous measurements of the spectral optical thickness can supplement aerosol properties derived from less frequent multi-angle sky radiance inversions (e.g., Dubovik and King, 2000; Dubovik et al., 2002).”
- Application of spheroid models to account for aerosol particle nonsphericity in remote sensing of desert dust (2006, background): “the optical depth [Eck et al., 1999; Reid et al., 1999; O’Neill et al., 2001; Schuster et al., 2006].”
- Variability and trends of aerosol properties over Kanpur, northern India using AERONET data (2001–10) (2012, methodology): “In contrast, a statistically significant difference is revealed for α380−500 with lower values during 2006–10, suggesting an increase in particle size of fine aerosols (Reid et al 1999, Schuster et al 2006).”
- Cosmic ray decreases affect atmospheric aerosols and clouds (2009, background): “Long wavelengths respond to their volume fraction, whilst short wavelengths are sensitive to the effective radius of the fine mode ( 250 nm) aerosol [Schuster et al., 2006].”
- Particulate emissions from commercial shipping: Chemical, physical, and optical properties (2008, background): “[2] The world shipping fleet consists of over 100,000 vessels larger than 100 gross tonnes [Corbett and Koehler, 2003], consumes up to 289 million tonnes of fuel per year [Corbett and Koehler, 2003; Endresen et al., 2003; Eyring et al., 2005a] and has estimated future growth of 2–6% a � 1 [Corbett e”