Articles | Volume 15, issue 10
https://doi.org/10.5194/acp-15-5947-2015
© Author(s) 2015. This work is distributed under
the Creative Commons Attribution 3.0 License.
the Creative Commons Attribution 3.0 License.
https://doi.org/10.5194/acp-15-5947-2015
© Author(s) 2015. This work is distributed under
the Creative Commons Attribution 3.0 License.
the Creative Commons Attribution 3.0 License.
Technical Note: Optical properties of desert aerosol with non-spherical mineral particles: data incorporated to OPAC
P. Koepke
CORRESPONDING AUTHOR
L-M-University Munich, Meteorological Institute, Theresienstr. 37, 80333 Munich, Germany
J. Gasteiger
L-M-University Munich, Meteorological Institute, Theresienstr. 37, 80333 Munich, Germany
M. Hess
DLR – German Aerospace Center, Remote-Sensing Technology Institute, Oberpfaffenhofen, 82234 Weßling, Germany
RASCIN, Thalkirchner Str. 284, 81371 Munich, Germany
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64 citations as recorded by crossref.
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- Machine learning algorithms for retrievals of aerosol and ocean color products from FY-3D MERSI-II instrument Y. Fan et al. 10.1016/j.jqsrt.2020.107042
- Deriving Aerosol Absorption Properties from Solar Ultraviolet Radiation Spectral Measurements at Thessaloniki, Greece I. Fountoulakis et al. 10.3390/rs11182179
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- Application of a high-temporal resolution model for the identification of columnar aerosol components F. Esposito et al. 10.1016/j.jastp.2019.105132
- Quantifying Uncertainties in OC-SMART Ocean Color Retrievals: A Bayesian Inversion Algorithm E. Pachniak et al. 10.3390/a16060301
1 citations as recorded by crossref.
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Latest update: 23 Nov 2024
Short summary
Desert dust particles in general are not spherical, which changes their scattering functions against that for spheres that often are used for remote-sensing and radiation budget investigations. In the new version of the data base OPAC (Optical Properties of Aerosols and Clouds), which easily allows one to model a large range of microphysical and optical aerosol properties for individually decided component mixtures, now typical non-spherical mineral particles are taken into account.
Desert dust particles in general are not spherical, which changes their scattering functions...
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