Higher Apparent Gas Transfer Velocities for CO(2) Compared to CH(4) in Small Lakes

[Image: see text] Large greenhouse gas emissions occur via the release of carbon dioxide (CO(2)) and methane (CH(4)) from the surface layer of lakes. Such emissions are modeled from the air–water gas concentration gradient and the gas transfer velocity (k). The links between k and the physical properties of the gas and water have led to the development of methods to convert k between gases through Schmidt number normalization. However, recent observations have found that such normalization of apparent k estimates from field measurements can yield different results for CH(4) and CO(2). We estimated k for CO(2) and CH(4) from measurements of concentration gradients and fluxes in four contrasting lakes and found consistently higher (on an average 1.7 times) normalized apparent k values for CO(2) than CH(4). From these results, we infer that several gas-specific factors, including chemical and biological processes within the water surface microlayer, can influence apparent k estimates. We highlight the importance of accurately measuring relevant air–water gas concentration gradients and considering gas-specific processes when estimating k.