RDPS, the Canadian Regional Deterministic Prediction System, is often less reliable for mid-level temperature evolution, especially 850 hPa warming events, compared to some peer models. RDPS tends to struggle with warm air advection aloft, particularly when the warming depends on subtle synoptic timing or shallow inversions. It has a known bias toward under-amplifying mid-level ridges and mixing warm layers too aggressively, which can delay or mute warming signals. That shows up most clearly in marginal setups like rain versus snow lines or freezing rain transitions.