Global warming has significantly altered plant growth patterns on the Tibetan Plateau (TP) over the past three decades. Plants adjust their growth trajectories in response to climate change, prioritizing leaf and stem growth or root extension to better absorb nutrients from the sun, atmosphere, or soil. Therefore, it is important to understand the mechanisms and dynamics of plant growth in permafrost regions of the TP, where significant amounts of carbon dioxide are absorbed, stored, and emitted.
