ECMWF and GFS ensemble outputs for Shenzhen on April 29 indicate a robust thermal advection pattern, pushing 850 hPa temperatures above seasonal norms. Surface response models consistently forecast peak daytime highs hitting 30-31°C, well clear of the 29°C threshold. Synoptic charts show a strengthening anticyclonic ridge, minimizing convective potential and locking in diurnal heating. This suggests no inversion layer will cap warming. We are positioning for a definitive breach. 95% NO — invalid if a late-developing cold front introduces significant cloud cover.