“…The Western region in Canada is dominated by the Prairie ecozone which occurs mostly between latitudes of 49° and 54°N, comprises more than 80% of the national agricultural land or 52 Mha (of which ∼60% is cropland), receives most of the N fertilizer used (∼75%) and grows nearly all the canola, spring wheat, and barley produced in Canada (Awada et al., 2021; Statistics Canada, 2016, 2022). The region is characterized by its aridity with an annual average precipitation ranging from 300 to 550 mm (McGinn, 2010) and long winters with approximately 150 soil freezing days and 5–15 freeze‐thaw cycles (Henry, 2008) There are five soil zones in this region (Brown, Dark‐brown, Black, Gray and Dark‐gray) with a general precipitation gradient along these soil types and contrasting soil organic matter values (higher for the Black zone at 5%–10% and lower for the Brown zone soils at 2%–5%) (Awada et al., 2021). The diversity in climatic and soil conditions implies that the drivers of freeze‐thaw cycle emissions and the importance of freeze‐thaw events to annual totals could vary considerably across the Prairies.…”