This study analyzed the characteristics and sources of aerosols in the Mt. Everest region from May to October 2022 based on instrumental observations and Potential Source Contribution Function (PSCF) analysis. Aerosols were classified into background-, coarse-, and fine-mode dominated types according to the PM₂.₅/PM₁₀ mass-ratio. Both coarse- and fine-mode aerosol increases were linked to low temperature and humidity, strong winds, and high single-scattering albedo (SSA), with black carbon (BC) showing the strongest positive correlation, indicating enhanced transport and reduced wet removal. The scattering and absorption Ångström exponents (SAE and AAE) effectively describe particle size and absorption feature, showing clear spectral signatures of dust-dominated scattering and carbonaceous absorption. The absorption and scattering coefficients of different aerosol modes decreased with increasing wavelength, whereas SSA increased with increasing wavelength, which was consistent with the optical behavior of dust in this region. PSCF analysis showed distinct source regions for each aerosol mode: coarse-mode aerosols mainly originated from northeastern and central India, whereas fine-mode aerosols were primarily transported from the Bay of Bengal. Although the Mt. Everest atmosphere is generally clean, it is strongly influenced by transboundary aerosols from South Asia. These results provide new insights into the physical, optical, and meteorological mechanisms governing regional and long-range pollution over high-altitude environments of the Tibetan Plateau.
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