Previous research has revealed that, during the late afternoon, the ozone (O3) concentration tends to elevate at the northern perimeter of Mount Everest (5200m above sea level). This increase is attributed to the natural gradient of rising O3 concentration with height, exacerbated by the corresponding downstream mountain winds. Our recent field observations corroborate this finding, showing a consistent increase in O3 concentrations by approximately 13.5±2.5 ppbv/km at a similar observational site. Despite these observations, the precise cause of this height-dependent increase in O3 remains elusive. In this study, we show that the influence of aerosol-photolysis interaction can partially explain the increment of O3 with height based on the field measurement results of the aerosol microphysical properties. Results show that the mean aerosol single scattering albedo, asymmetry factor, scattering angstrom index, and absorption angstrom index on the edge of the Mountain Everest were 0.98, 0.70, 1.3, and 0.66 respectively. The photolysis ratio increases with the height based on the tropospheric ultraviolet and visible model simulations with the measured aerosol optical properties. Sensitivity experiments further demonstrate that the unique microphysical properties of aerosols at Mount Everest result in a higher increment rate of the nitrate oxide photolysis rate with height (1.93×10-3/kms) compared to those observed in Beijing (1.53×10-3/kms). This difference leads to an additional increase in ozone concentration by 1.8 ppbv (from 69.1 ppbv to 70.9 ppbv) at the top of the boundary layer. Our study underscores the significant impact of aerosol-photolysis interactions on ozone concentrations and offers insights that could potentially advance our understanding of the sources of ozone in the upper troposphere over the Tibetan Plateau.
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