Biogenic emission of dimethyl sulfide (DMS) from seawater is the major natural source of sulfur into the atmosphere. In this study, we use an advanced air quality model (CMAQv5.2) with DMS chemistry to examine the impact of DMS emissions from seawater on summertime air quality over China. A national scale database of DMS concentration in seawater is established based on a 5-year observational record in the East China seas including the Bohai Sea, the Yellow Sea, and the East China Sea. We employ a commonly used global database and also the newly developed local database of oceanic DMS concentration, calculate DMS emissions using three different parameterization schemes, and perform five different model simulations for July, 2018. Results indicate that in large coastal areas of China, the average DMS emissions flux obtained with the local database is 3 times higher than that resulting from the global database, with a mean value of 9.1 μmol m −2 day −1 in the Bohai Sea, 8.4 μmol m −2 day −1 in the Yellow Sea, and 13.4 μmol m −2 day −1 in the East China Sea. The total DMS emissions flux calculated with the Nightingale scheme is 42% higher than that obtained with the Liss and Merlivat scheme but is 15% lower than that obtained with the Wanninkhof scheme. Among the three parameterizations, results of the Liss and Merlivat scheme agree better with the ship-based observations over China's coastal waters. DMS emissions with the Liss and Merlivat parametrization increase atmospheric sulfur dioxide (SO 2) and sulfate (SO 4 2−) concentration over the East China seas by 6.4% and 3.3%, respectively. Our results indicate that although the anthropogenic source is still the dominant contributor of atmospheric sulfur burden in China, biogenic DMS emissions source is nonnegligible. SO 4 2− is the main component of atmospheric particulate matter that can participate in cloud formation, affecting atmospheric radiation balance and climate (Charlson et al., 1987). Despite the substantial progress made during the last 30-40 years, the specific DMS oxidation pathways are still not very well understood (Barnes et al., 2006; Hoffmann et al., 2016; Ravishankara et al., 1997). The reaction of hydroxyl radical (OH) with DMS is perhaps the most studied of all reactions involving DMS and is one of the most complex reactions as OH radical both adds to and abstracts from DMS. Contrary to abstraction, the rate of the addition reaction increases with decreasing temperature (Atkinson et al., 2004; Zhu et al., 2006). The reaction of DMS with nitrate radical (NO 3) is important at night and in the polluted atmosphere (Stark et al., 2007). Nevertheless, halogens contribute significantly to DMS oxidation, which are ignored in many air quality models. Noteworthy is the reaction of DMS with bromine oxide (BrO), which could be particularly important as a sink for DMS especially when BrO mixing ©2020 The Authors. This is an open access article under the terms of the Creative Commons Attribution-NonCommercial-NoDerivs License, which permits use and distribu...