The AODs at different wavelengths are mutually connected by the following equation:
AOD(wl_2)/AOD(wl_1) = (wl_1/wl_2)^A
where wl_x denotes the wavelength. A denotes the Ångström exponent. More details could be found in Marseille et al.(2011), The definition of an atmospheric database for Aeolus
Thanks for your reply. This works for the determination of normal AOD at given wavelength with respect to known normal AOD at the other wavelength using the Ångström exponent . But, I meant the conversion of normal AOD to deep blue AOD.