Preprint Article Version 1 Preserved in Portico This version is not peer-reviewed

Sensitivity of Radiative Fluxes to Aerosols in the ALADIN-HIRLAM Numerical Weather Prediction System

Version 1 : Received: 16 January 2020 / Approved: 17 January 2020 / Online: 17 January 2020 (09:53:01 CET)

A peer-reviewed article of this Preprint also exists.

Rontu, L.; Gleeson, E.; Martin Perez, D.; Pagh Nielsen, K.; Toll, V. Sensitivity of Radiative Fluxes to Aerosols in the ALADIN-HIRLAM Numerical Weather Prediction System. Atmosphere 2020, 11, 205. Rontu, L.; Gleeson, E.; Martin Perez, D.; Pagh Nielsen, K.; Toll, V. Sensitivity of Radiative Fluxes to Aerosols in the ALADIN-HIRLAM Numerical Weather Prediction System. Atmosphere 2020, 11, 205.

Abstract

The direct radiative effect of aerosols is taken into account in many limited area numerical weather prediction models using wavelength-dependent aerosol optical depths of a range of aerosol species. We study the impact of aerosol distribution and optical properties on radiative transfer, based on climatological and more realistic near real-time aerosol data. Sensitivity tests were carried out using the single column version of the ALADIN-HIRLAM numerical weather prediction system, set up to use the HLRADIA broadband radiation scheme. The tests were restricted to clear-sky cases to avoid the complication of cloud-radiation-aerosol interactions. The largest differences in radiative fluxes and heating rates were found to be due to different aerosol loads. When the loads are large, the radiative fluxes and heating rates are sensitive to the aerosol inherent optical properties and vertical distribution of the aerosol species. Impacts of aerosols on shortwave radiation dominate longwave impacts. Sensitivity experiments indicated the important effects of highly absorbing black carbon aerosols and strongly scattering desert dust.

Keywords

aerosols; CAMS; NWP; ALADIN-HIRLAM; MUSC; direct radiative effect

Subject

Environmental and Earth Sciences, Atmospheric Science and Meteorology

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