Impacts of South Asian aerosol inflow over Mount Qomolangma on downstream cloud–precipitation processes through a long-range ice-crystal “seeding” effect

Mount Qomolangma (MQ) serves as a natural laboratory for investigating aerosol–cloud–precipitation interactions over the Tibetan Plateau (TP). Using satellite and comprehensive ground-based observations, we identify pronounced ice-cloud activation associated with transported exogenous aerosols. Under different large-scale atmospheric circulation regimes, ice-phase cloud activated over MQ can be efficiently transported downstream through distinct pathways, exerting a pronounced ice crystal seeding effect on cloud–precipitation conversion. The spatial patterns of these downstream pathways are highly consistent with regions of enhanced ice-phase occurrence, precipitation, and upper-tropospheric latent heat release. This study provides new insight into the downstream impacts of aerosol transport through ice seeding for cloud precipitation. The findings highlight the important role of aerosol-induced ice-phase processes in modulating cloud and precipitation systems over the “Third Pole” and its downstream regions, with significant implications for understanding downstream extreme precipitation and environment change under South Asian increasing anthropogenic influences.