Shale reservoirs commonly contain water, and studying the gas adsorption behavior and thermodynamic characteristics in wet shale is of great significance for shale gas resource evaluation and development. However, the influence of water molecules on the adsorption behavior and thermodynamics of methane adsorption in shales remains poorly understood. In this study, we considered the adsorption mechanism and occurrence environment of methane in shale, constructed an adsorption model that considers the combined effects of moisture and temperature, and verified the rationality of the newly constructed adsorption model from a considerable amount of published data. Then, combining the adsorption potential theory and real gas behavior, the absolute isothermal adsorption curves at various temperatures were successfully calculated using the global fitting method, and the mechanism of gas adsorption under the coupling of multiple factors was studied. On this basis, a rigorous framework for analyzing the adsorption thermodynamic characteristics of methane in shale was proposed, and the mechanism of the influence of water on methane gas adsorption was deeply studied, and the adsorption behavior of methane gas in aqueous shale was further analyzed. The results revealed that moisture had a significant inhibitory effect on the adsorption capacity of shale, and the methane adsorption amount decreases with the increase of moisture content. Similarly, temperature has an inhibitory effect on shale adsorption capacity. However, the effect of moisture and temperature on gas adsorption capacity was synergistic and negative, with high pressure helping to reduce the impact of humidity on methane adsorption capacity in terms of gas content. The thermodynamic model concluded that methane adsorbed in dry and wet shale was physical adsorption, with the isosteric heat of adsorption dropping and accompanying an increase in water content and temperature. The increase in water content led to a decrease in the absolute value of the isosteric entropy of adsorption, which proved to be not conducive to forming a stable and orderly arrangement of methane molecules on the shale surface. Water will preferentially occupy high-energy adsorption sites in micropores and hydrophilic water points in mesopores and macropores and fill micropores and some mesopores under capillary condensation as the water content increases. Water molecules on the methane adsorption basically functioned by modifying the interactions between the adsorbate and the adsorbent. The findings of this study can help for better understanding of subsurface supercritical adsorption under reservoir conditions and provide a basis for shale gas's resource assessment and optimal extraction.