Vertical profile of the clear-sky aerosol direct radiative effect in an Alpine valley, by the synergy of ground-based measurements and radiative transfer simulations

نویسندگان

چکیده

Abstract Atmospheric aerosols play an important role in Earth’s radiative balance, directly interacting with solar radiation or influencing cloud formation and properties. In order to assess their impact, it is necessary accurately characterise optical properties, together spatial vertical distribution. The information on aerosol profile often scarce, particular mountainous, complex terrains. This study presents the first attempt evaluate shortwave direct effect Aosta Valley, a mountainous region Northwestern Italian Alps. Ground-based, remote sensing instruments (a sky radiometer Automated Lidar Ceilometer) are used derive two descriptions of properties distribution: first, more accurate description, which includes whole spectral about extinction coefficient, phase function single scattering albedo; second, approximate one, only relies spectrally constant values albedo asymmetry factor. as input for transfer simulations, allow estimate, cloudless conditions, instantaneous heating rates lower layers atmosphere. simulations obtained do not differ significantly: they highlight strong surface dimming (between − 25 50 W m 2 ) due presence aerosol, considerable absorption inside atmospheric column (around + 30 ), overall small cooling Earth-atmospheric system. within leads up 1.5 K day 1 tropospheric below 6 km a.s.l. These results show that, some can be even this Alpine environment, usually considered relatively pristine (yearly average PM 10 concentration 20 μg 3 ).

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ژورنال

عنوان ژورنال: Bulletin of Atmospheric Science and Technology

سال: 2021

ISSN: ['2662-1495', '2662-1509']

DOI: https://doi.org/10.1007/s42865-021-00041-w