Distributions and fluxes of methane were determined during two surveys in March--May 2001 in the Yellow Sea and the East China Sea. Methane concentrations in the surface and bottom waters range from 2.52 to 5.48 and 2.81 to 8.17 nM, respectively. The distributions of methane are influenced obviously by the Yangtze River effluent and Kuroshio water. CH4 input via the Yangtze River is estimated to be 3.17 mol/s, of which a considerable part may be lost by air-sea exchange during estuarine mixing. Net CH4 flux exported from the shelf to the Kuroshio is about 1.84 mol/s. Methane enrichments in bottom waters occur widely, which reveals sediment sources of CH4. However, the CH4 input from the sediments of the studied region in spring is lower than other shelf regions due to low organic carbon in the sediments and high O2 contents in the water column. The sea-to-air methane fluxes are estimated to be 1.36 ¿ 1.45 and 2.30 ¿ 2.36 ¿mol m-2 d-1 using Liss and Merlivat <1986> and Wanninkhof <1992> relationships, respectively, and the estimated spring emission rate of methane ranges from 9.32 ¿ 10-3 to 15.7 ¿ 10-3 Tg CH4 yr-1. However, these estimations suffer from the neglect of seasonal variability and should be taken as a low limit. Therefore more measurement campaigns should be carried out to enhance our understanding of this particular oceanic region.