Aerosol radiative forcing efficiency in the UV-B region over central Argentina
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文摘

The direct UV-B radiative forcing at surface varies between − 1.76 and − 0.11 Wm–2.

Single scattering albedo is an important parameter in the UV-B forcing.

UV-B radiative forcing is larger for absorbing particles and smaller solar zenith angle.

Good agreement between surface and satellite estimations of radiative forcing is observed.

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