6533b82bfe1ef96bd128e0b1
RESEARCH PRODUCT
Ground-based measured and calculated spectra of actinic flux density and downward UV irradiance in cloudless conditions and their sensitivity to aerosol microphysical properties
Markus FiebigManfred WendischUwe FeisterE. EcksteinThomas TrautmannThomas TrautmannBarbara Frühsubject
Atmospheric ScienceMaterials scienceParticle numberIrradianceSoil ScienceAquatic ScienceOceanographyAtmospheric sciencesSpectral lineOpticsGeochemistry and PetrologyEarth and Planetary Sciences (miscellaneous)Radiative transferUV irradiancePhysics::Atmospheric and Oceanic Physicsactinic fluxEarth-Surface ProcessesWater Science and Technologyradiative transfer simulationstransmission and scattering of radiationEcologybusiness.industryPaleontologyForestryaerosols and particlesAerosolWavelengthGeophysicsSpace and Planetary ScienceParticle-size distributionParticlebusinessaerosol radiative forcingdescription
Ground-based spectral measurements of actinic flux density (300–660 nm wavelength) and downward UV irradiance (300–324 nm) under cloudless conditions have been compared with the results of one-dimensional radiative transfer calculations employing concurrent airborne vertical profile measurements of aerosol particle size distributions. Good agreement (within ±10%) between measured and calculated spectra was found. The remaining differences were explained by uncertainties inherent in the aerosol particle microphysical input data and the column ozone content. A respective sensitivity analysis of the calculated spectra, which was based on the observed variability of microphysical properties, has shown that the particle number concentration is the most crucial input uncertainty for both the actinic flux density and the UV irradiance. For the wavelength range investigated, the uncertainty of the column ozone content is of minor importance for both spectral quantities.
year | journal | country | edition | language |
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2003-01-01 | Journal of Geophysical Research |