Despite differences between the cover crop growth and decomposition phases, few greenhouse gas (GHG) studies have separated these phases from each other. This study's hypothesis was that a living cover crop reduces soil inorganic N concentrations and soil water, thereby reducing N 2 O emissions. We quantified the effects of a fall-planted living cereal rye (Secale cereale L.) cover crop (2017, 2018, 2019) on the following spring's soil temperature, soil water, water-filled porosity (WFP), inorganic N, and GHG (N 2 O-N and CO 2 -C) emissions and compared these measurements to bare soil. The experimental design was a randomized complete block, where years were treated as blocks. Rye was fall planted in 2017, 2018, and 2019, but mostly emerged the following spring. The GHG emissions were near-continuously measured from early spring through June. Rye biomass was 1,049, 428, and 2,647 kg ha -1 in 2018, 2019, and 2020, respectively. Compared to the bare soil, rye reduced WFP in the surface 5 cm by 29, 15, and 26% in 2018, 2019, and 2020 and reduced soil NO 3 -N in surface 30 cm by 53% in 2019 (p = .04) and 65% in 2020 (p = .07), respectively. Rye changed the N 2 O and CO 2 frequency emission signatures. It also reduced N 2 O emissions by 66% but did not influence CO 2 -C emissions during the period prior to corn (Zea mays L.) emergence (VE). After VE, rye and bare soils N 2 O emissions were similar. These results suggest that nitrous oxide (N 2 O-N) sampling protocols must account for early season impacts of the living cover.