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- W15702949 abstract "In the upper troposphere and lower stratosphere, cosmic rays create Be7 atoms, which subsequently attach to submicron dust particles, so that wet deposition ultimately removes most Be7 from troposphere. The Be7 concentration at ground level and the wet deposition strongly depend on the vertical turbulent diffusion in the atmospheric boundary layer. Because this source is well known,and because there is a large climatological data set for Be7 concentration in surface air and deposition on the surface simulating, Be7 provides a good tool to test the wet scavenging and turbulent diffusion coefficient parameterizations. A numerical solution of the diffusion equation is obtained for the vertical diffusion of Be7 for different parameterizations of the turbulent diffusion coefficient taken from literature. A comparison is made with the concentration at the surface and wet deposition measurements obtained at the National Institute of Meteorology and Hydrology, Romania. The parameterization of the turbulent diffusion coefficient gives the best fit with the measurements for different weather conditions and different stability conditions of the atmospheric boundary layer." @default.
- W15702949 created "2016-06-24" @default.
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- W15702949 date "1996-01-01" @default.
- W15702949 modified "2023-10-14" @default.
- W15702949 title "Vertical diffusion simulation of Be7 at midlatitudes" @default.
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- W15702949 doi "https://doi.org/10.1016/b978-008042030-1/50088-3" @default.
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