Variability of aerosol optical properties derived from in situ aircraft measurements during ACE‐Asia
By T. Anderson, S. Masonis, D. Covert, N. Ahlquist, S. Howell, A. Clarke, C. McNaughton. 2003
206 citations recorded by the source corpus.
Subfields: Atmospheric Science, Global and Planetary Change, Health, Toxicology and Mutagenesis
View Paper: https://www.semanticscholar.org/paper/de5cf3c494192e80e2b7273f615698877c127628
How researchers see this paper
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In Atmospheric Science
- Albert Ansmann
- Dietrich Althausen
- Detlef Müller
- A. Ravishankara
- A. Pettersson
- R. Weber
- Volker Freudenthaler
- Ina Mattis
In Global and Planetary Change
- Albert Ansmann
- Dietrich Althausen
- Detlef Müller
- Volker Freudenthaler
- Ina Mattis
- Ulla Wandinger
- D. Lack
- Anatoli Chaikovsky
In Health, Toxicology and Mutagenesis
Citations in the corpus
- Multiyear aerosol observations with dual‐wavelength Raman lidar in the framework of EARLINET (2004, background): “In Southeast and East Asian aerosol plumes lidar ratios were mainly between 40 and 60 sr at 500–550 nm [Franke et al., 2001; Anderson et al., 2003 ].”
- Aerosol-type-dependent lidar ratios observed with Raman lidar (2007, methodology): “In agreement with our PRD observations, Anderson et al. [2003] found a mean lidar ratio of 45 ± 10 sr at 532 nm as mean value during the ACE-Asia campaign in the spring of 2000.”
- EARLINET correlative measurements for CALIPSO: First intercomparison results (2010, background): “[56] Mesoscale variation of tropospheric aerosol has been extensively discussed by Anderson et al. [2003], starting from correlation analysis of measurements of high‐resolution column‐integrated optical properties.”
- Characterization of iron oxides in mineral dust aerosols: Implications for light absorption (2006, methodology): “On the basis of in situ measurements of scattering and absorption coefficients conducted from the NCAR C-130 aircraft during the ACE-Asia field experiment, Anderson et al. [2003] found !0 of 0.96 (±0.01) at 550 nm for dust particles in the coarse size mode (aerodynamic-equivalent diameter is highe”
- Size distributions and mixtures of dust and black carbon aerosol in Asian outflow: Physiochemistry and optical properties (2004, methodology): “The latter was measured using a 1 mm aerodynamic impactor [Anderson et al., 2003].”
- Aerosol Absorption Measurement using Photoacoustic Spectroscopy: Sensitivity, Calibration, and Uncertainty Developments (2006, methodology): “The works by Bond et al. (1999) , Anderson et al.”