The long-range transport of naturally occurring and anthropogenic aerosols originating from Asian deserts and megacities, respectively, can have a significant impact on the biogeochemical cycling of metals in the Fe-limited, high nutrient-low chlorophyll (HNLC) region of the northeast (NE) subarctic Pacific Ocean. These aerosols can deposit essential (e.g., Fe) and possibly toxic (e.g., Cu) metals to surface waters
thereby affecting micronutrients' bioavailability, and ultimately primary productivity in this region. In this study, we aimed to determine the provenance and spatiotemporal trends of metal inputs from Asian aerosol outflows into the NE Pacific Ocean. To do so, we collected aerosols on six research cruises along the Line P transect (GEOTRACES GPpr07), across three seasons in four years. Lead isotopic composition signatures were less radiogenic (high