In semi-arid mountainous watersheds, nitrogen (N) and phosphorus (P) export mechanisms vary across hydrological periods and year types, yet remain insufficiently characterized, which hampers adaptive non-point source (NPS) control and can elevate event-driven nutrient pulses and downstream eutrophication risk. This study investigates the Qingshuihe River Basin in North China using hydrological and water quality data from the rainy seasons of 2019 (dry), 2020 (wet), and 2023 (normal), together with 2023 snowmelt observations, and applies concentration-discharge (C-Q) models to identify N and P export behaviors. Clear seasonal shifts in nutrient forms and limitation types were observed. During the rainy season, N was dominated by dissolved forms (similar to 80%), whereas P was primarily particulate (similar to 70%). During snowmelt, N shifted to TON (71%), while particulate P decreased to 65%. N export exhibited transport limitation in the dry year, source limitation in the wet year, and transitional behavior in the normal year. P showed strong transport limitation in the dry year, weaker transport limitation in the normal year, and weak source limitation in the wet year, driven by dilution under extreme precipitation and altered flow pathways. During snowmelt, N showed weak source limitation, whereas P consistently displayed sediment-driven transport limitation. These results reveal hydrological-regime-dependent N and P export dynamics and underscore the need for hydrological-year-type-based, period-specific "source-process" management strategies. The findings provide a process-based basis for improving NPS pollution mitigation in semi-arid mountainous regions.