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Climate change might alter annual snowfall patterns and modify the duration and magnitude of snow cover in temperate regions with resultant impacts on soil microclimate and soil   CO 2    efflux ( F   soil  ). We used a 5‐year time series of  F   soil   measurements from a mid‐elevation forest to assess the effects of naturally changing snow cover. Snow cover varied considerably in duration (105–154 days) and depth (mean snow depth 19–59 cm). Periodically shallow snow cover (<10 cm) caused soil freezing or increased variation in soil temperature. This was mostly not reflected in  F   soil   which tended to decrease gradually throughout winter. Progressively decreasing C substrate availability (identified by substrate induced respiration) likely over‐rid the effects of slowly changing soil temperatures and determined the overall course of  F   soil  . Cumulative   CO 2    efflux from beneath snow cover varied between 0.46 and 0.95 t C ha −1  yr −1  and amounted to between 6 and 12% of the annual efflux. When compared over a fixed interval (the longest period of snow cover during the 5 years), the cumulative   CO 2    efflux ranged between 0.77 and 1.18 t C ha −1  or between 11 and 15% of the annual soil   CO 2    efflux. The relative contribution (15%) was highest during the year with the shortest winter. Variations in snow cover were not reflected in the annual   CO 2    efflux (7.44–8.41 t C ha −1 ) which did not differ significantly between years and did not correlate with any snow parameter. Regional climate at our site was characterized by relatively high amounts of precipitation. Therefore, snow did not play a role in terms of water supply during the warm season and primarily affected cold season processes. The role of changing snow cover therefore seems rather marginal when compared to potential climate change effects on  F   soil   during the warm season.

Natural variations in snow cover do not affect the annual soil CO 2 efflux from a mid‐elevation temperate forest