Fluxes of CO₂ and CH₄ through a seasonal snowpack were measured in and adjacent to a subalpine wetland in Rocky Mountain National Park, Colorado. Gas diffusion through the snow was controlled by gas production or consumption in the soil and by physical snowpack properties. The snowpack insulated soils from cold midwinter air temperatures allowing microbial activity to continue through the winter. All soil types studied were net sources of CO₂ to the atmosphere through the winter, whereas saturated soils in the wetland center were net emitters of CH₄ and soils adjacent to the wetland were net CH₄ consumers. Most sites showed similar temporal patterns in winter gas fluxes; the lowest fluxes occurred in early winter, and maximum fluxes occurred at the onset of snowmelt. Temporal changes in fluxes probably were related to changes in soil-moisture conditions and hydrology because soil temperatures were relatively constant under the snowpack. Average winter CO₂ fluxes were 42.3, 31.2, and 14.6 mmol m⁻² d⁻¹ over dry, moist, and saturated soils, respectively, which accounted for 8 to 23% of the gross annual CO₂emissions from these soils. Average winter CH₄ fluxes were −0.016, 0.274, and 2.87 mmol m⁻² d⁻¹over dry, moist, and saturated soils, respectively. Microbial activity under snow cover accounted for 12% of the annual CH₄ consumption in dry soils and 58 and 12% of the annual CH₄ emitted from moist and saturated soils, respectively. The observed ranges in CO₂ and CH₄ flux through snow indicated that winter fluxes are an important part of the annual carbon budget in seasonally snow-covered terrains.