Using OMPS-LP color ratio to extract stratospheric aerosol particle size and concentration with application to volcanic eruptions.

We develop an algorithm that uses the aerosol extinction at two wavelengths (color ratio) to derive the size and number density for stratospheric aerosols. We apply our algorithm to Ozone Mapping Profiler Suite Limb Profiler (OMPS-10 LP) L2 and Stratospheric Aerosol and Gas Experiment (SAGE) data. We show that the color ratio between two wavelengths (e.g. 510 nm/869 nm) is insensitive to aerosol concentration and thus can be used to derive aerosol size assuming a log-normal size distribution. With the size and the extinction, we can compute a number density consistent with both wavelengths. Our results compare favorably to balloon borne particle size and concentration measurements. Our results are also consistent with SAGE solar occultation measurements. Finally, we show the background distribution of stratospheric aerosols and the changes 15 in those distributions during the Reikoke and Hunga Tonga-Hunga Ha'apai volcanic eruptions. We also show the evolution of the size and number density of aerosols following both of those eruptions. [ABSTRACT FROM AUTHOR]