2007•Unpublished venueRequires access

Aerosol scattering and mass concentration for different aerosol types

F. Wagner, Nuno Belo

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Abstract

m 2 g -1 and the later values between 2.5 - 3 m 2 g -1 . The difference is more visible as the aerosol load increases and so do PM10 and σ550. During the continental polluted period (likely a mixture with desert dust aerosols) the mass scattering efficiency values exhibited higher variability and range from 1 up to 3 m 2 g -1 . The mass scattering efficiencies for the

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m 2 g -1 and the later values between 2.5 - 3 m 2 g -1 . The difference is more visible as the aerosol load increases and so do PM10 and σ550. During the continental polluted period (likely a mixture with desert dust aerosols) the mass scattering efficiency values exhibited higher variability and range from 1 up to 3 m 2 g -1 . The mass scattering efficiencies for the

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Available abstract

m 2 g -1 and the later values between 2.5 - 3 m 2 g -1 . The difference is more visible as the aerosol load increases and so do PM10 and σ550. During the continental polluted period (likely a mixture with desert dust aerosols) the mass scattering efficiency values exhibited higher variability and range from 1 up to 3 m 2 g -1 . The mass scattering efficiencies for the

Key concepts: Aerosol, Mass concentration (chemistry), Atmospheric sciences, Environmental science, Scattering, Range (aeronautics), Environmental chemistry, Meteorology

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