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- W4300102857 abstract "The optical properties of aerosols are subject of many experimental and theoretical studies. One of these properties is the aerosol optical depth (AOD), a vertical integrated value for the aerosol content in the atmosphere. In cooperation with the Remote Sensing Group at the Institute of Geography of the University of Berne, AOD data derived from TERRA/MODIS measurements were compared with numerical simulations for selected weather situations. Additionally, we use our AERONET sunphotometer station data for comparison the simulations.The model system KAMM/DRAIS/MADEsoot (Adrian and Fiedler, 1991; Vogel et al., 1995; Riemer et al., 2003) is used to simulate the three-dimensional and time-dependent distributions of physical and chemical variables. The non-hydrostatic model KAMM gives the meteorological variables in the model domain which is situated in South-Western Germany. The module DRAIS simulates the transport and diffusion of reactive chemical species. The gas-phase chemistry is computed with a modified RADM2 mechanism (Stockwell et al., 1990). The aerosol model MADEsoot (Riemer et al., 2003) which is based on the aerosol model MADE (Ackermann et al., 1998; Schell et al., 2001), is used to calculate the spatial and temporal distribution of aerosol particles. The size distributions and the chemical composition of the particles are taken into account. The aerosol particles are described by five individual modes. The optical properties as the extinction coefficient, the single scattering albedo, and the phase function in terms of Legendre polynomials are calculated for each grid box applying Mie theory using a code according to Bohren and Huffman (1983).The results will be presented and especially the differences between the satellite, AERONET data and the numerical simulations will be shown." @default.
- W4300102857 created "2022-10-03" @default.
- W4300102857 date "1834-11-01" @default.
- W4300102857 modified "2023-10-01" @default.
- W4300102857 title "Meteorological observations for September, 1834" @default.
- W4300102857 doi "https://doi.org/10.1016/s0016-0032(34)91095-4" @default.
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