To better understand the physicochemical evolution of Asian dust particles during long-range transport, water-soluble organic compounds (WSOCs) in gas- (WSOCg) and particle-phase (WSOCp) in the spring atmosphere of Shanghai during the 2023 dust storm period (DS) and haze events (HE) were simultaneously measured with a 3 h time resolution, and characterized for their optical properties and size distribution. Our results showed that gas-to-particle-phase partitioning coefficients (F-p) of WSOCs in DS (0.30 +/- 0.06) was comparable to that in HE (0.32 +/- 0.06), although both temperature and relative humidity in DS were not favorable for the partitioning, indicating a promoting role of dust particles in the transformation process of WSOCg from gas to particle phase. F-p variation was largely driven by aerosol liquid water content in HE but by aerosol acidity in DS. WSOCp and its light absorption at lambda(365 nm) dominated at the fine mode (< 2.1 m) in non-DS period and the coarse mode (> 2.1 mu m) in DS, respectively. Mass absorption coefficient (MAC) of the coarse mode of WSOCp at lambda(365 nm) in DS was 0.8 m(2) g(-1), which is four times that (0.20 +/- 0.09 m(2) g(-1)) in the source region of Tengger Desert, suggesting a remarkably increase in light absorbing ability of Asian dust during long-range transport. Sharp co-increases of nitroaromatics, imidazoles, and water-soluble organic nitrogen at the coarse mode in the DS period further revealed that such an increasing MAC is mainly caused by adsorption and heterogeneous formation of light absorbing nitrogen-containing organics on the dust surface during long-range transport.