Abstract
Anthropogenic warming has intensified extreme climate events, yet whether vegetation phenology in subtropical transitional zones follows the canonical warming-advance relationship or deviates under extreme conditions remains unresolved. Here, we analyze MODIS NDVI and ETCCDI extreme climate data across the northern slope of the Nanling Mountains, a critical subtropical transitional zone in southern China. At the spatial and interannual scale, SOS correlates negatively with extreme warm indices across 65.97% of the study area, i.e., warmer conditions coincide with earlier (canonical warming-advance) SOS, yet the regional SOS trend is non-significant despite coherent warming. We propose that heat-stress dormancy, extreme spring warmth triggering a reversible quiescent response that overrides thermal-time accumulation, is the most plausible explanation, although the present correlative, remote-sensing design cannot yet establish the underlying physiological mechanism. Growing season lengthening is driven by EOS delay (6.4 d per four years, p < 0.05) rather than SOS advance. Extreme precipitation is also predominantly associated with earlier SOS, with 75%–80% of pixels showing significant negative correlations, indicating that both thermal and moisture extremes shape spring phenology. Vegetation types follow a sensitivity hierarchy: cultivated land and grassland show the strongest phenological shifts, while natural forests remain buffered. These findings qualify the universal applicability of the warming-advance framework and call for incorporating heat-stress dormancy into phenological projections for subtropical transitional zones under continued extreme warming.