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Yu et al. (1) reported that the beginning of vegetation growing season (BGS) of the alpine steppe and meadow on the Tibetan Plateau was delayed since the mid-1990s under warming winter and spring (1). They wrote that “this delay appeared to be related to later fulfillment of chilling requirements,” and they suggested that “continued warming may strengthen this effect or even reverse the advancing trend in spring phenology” (1). This idea was proposed earlier for phenology of some species (2) and was tested on the alpine vegetations at the regional level. Using this idea, if winter warming continues and spring warming does not accelerate, the delaying trend should continue. We found, however, that, despite the continued winter warming and the fluctuating spring temperature (Tspring is the …

Spring phenology was not consistently related to winter warming on the Tibetan Plateau