The QTP has already experienced an earlier and faster warming process, which is expected to continue at an accelerated pace in the future [ 4 , 5 ], with the regional climate exhibiting a marked trend towards warmer and wetter conditions [ 6 , 7 ].
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Centroid Migration and Distribution of Dominant Species in Different Grassland Types Revealing Climate Change Responses on the Qinghai-Tibet Plateau.
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Under the SSP2-4.5 and SSP5-8.5 scenarios, the overlap in the potential distribution of the three dominant species in alpine meadows exhibits an increasing trend from southeast to northwest.