Microseepage is likely the most important geological source of methane, globally estimated to be in the order of 10-24 Tg yr −1 , followed by macro-seepage emissions such as mud volcanoes, gas-oil seeps, and submarine seeps (Etiope & Klusman, 2010;. Many studies show that (a) hydrocarbon microseepage dominantly occurs in correspondence with petroleum fields (mostly gas fields), and in particular along the faulted boundaries of the reservoirs (Ciotoli et al., 2020;Macgregor, 1993), and (b) that the gas flux to the atmosphere is higher in winter and lower in summer, in relation to temperature-driven methanotrophic consumption (Etiope & Klusman, 2010;Klusman, 2003). Methane flux data are however available only from a few petroleum provinces (mostly in central United States, Italy, Romania, and China) and their seasonal variation is scarcely known. The actual global area of microseepage is, then, only theoretically predictable and the emission factors, which are essential for bottom-up emission estimates, have relatively high uncertainty Saunois et al., 2020). In particular, there are no sufficient data showing the effect of ice content in the soil in winter. Although methanotrophic consumption is lower in winter, leading to enhanced methane release to the atmosphere, in some regions the presence of ice may reduce the gas exhalation (as observed in permafrost regions; e.g., O'Connor et al., 2010), inverting the seasonal trend.