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During the spring of 2021, rapid surface cooling in the Arctic area expanded to most of the East Asian region, featuring surface-temperature dipole patterns of the colder west (Mongolia and northern-central China) and the warmer east (eastern-northeastern China, the Yellow Sea, and Korea). Despite the decreasing trend of dusty days within Korea, a notable rise in the occurrence of transboundary mineral dust-induced dusty days was observed in contributing to an increase in PM 10 levels in the spring of 2021. This study investigated the PM 10 source apportionment of anthropogenic dust, mineral dust, and biomass burning in the East Asian region and its transboundary impact on Korea, within the context of the surface-temperature dipole pattern observed in April of 2021. Source apportionment of PM 10 was determined through a comparative analysis between baseline and sensitivity experiments conducted by means of a WRF-Chem simulation. In these sensitivity simulations, emissions from each source were systematically excluded to assess their individual contributions. PM 10 Base refers to baseline simulations, PM 10 Anthro to anthropogenic emissions, PM 10 Dust to mineral dust, and PM 10 Biomass to biomass burning. The colder west pattern was linked to increased synoptic-scale cyclonic activity, marked by higher positive potential vorticity, causing a sudden surge in severe dust storms over Mongolia and northern China. PM 10 Base levels were most elevated in the higher terrain of Mongolia, comprising predominantly PM 10 Dust (95%). However, the dominance of atmospheric-warming-induced anticyclones, represented by enhanced negative potential vorticity, prevailed over the lower terrain in the warmer east regions, obstructing the transboundary dispersion of PM 10 Base to Korea. Nevertheless, Korea experienced a transboundary contribution of PM 10 Dust , reaching 35%. In addition, the source apportionments indicated a PM 10 Anthro ratio of 55% in eastern China and a PM 10 Biomass ratio of 35% in northeastern China, contributing 25% and 5% respectively to Korea. During April 14–30, 2021, the dipole pattern evolved further to the significantly colder west (Mongolia and China) and the moderately warmer east (the Yellow Sea and Korea). The transboundary contributions of PM 10 Anthro , PM 10 Dust , and PM 10 Biomass were intensified as a composite mixture within Korea, an outcome attributed to the intermittent cyclones and subsequent anticyclones. • Dusty days fell in Korea, but mineral dust surged, raising PM 10 in spring 2021. • Arctic spring cooling led to an East Asian cold-west, warm-east dipole pattern. • The colder west amplified cyclones, sparking dust storms in Mongolia and China. • Warming-induced anticyclones obstructed the transboundary dispersion of mineral dust. • Dust from eastern-northern China impacted Korea's PM 10 in a warm anticyclone. [ABSTRACT FROM AUTHOR]