Method for Estimating the Highest Specific Methane Flux from the Surface of Reservoirs

This paper summarizes the results of the database of changes in the specific methane flux at various types of water reservoirs in Russia in which the authors participated. Measurements were carried out by the method of floating chambers in different periods of the annual hydroecological cycle. A comparison of the data with the results of foreign experience is given. An approach to the parameterization of specific methane flux for calculating the maximum possible methane emission from artificial reservoirs when developing quantitative quotas of greenhouse gas emissions is proposed. The estimation both in different phases of regime (stratification and homothermia) and for separate morphological parts of reservoirs differing in depth is offered.