Abstract:<p>The vegetation&#8217;s response to climate change is a major source of uncertainty in terrestrial biosphere model (TBM) projections. Constraining carbon cycle feedbacks to climate change requires improving our understanding of both the direct plant physiological responses to global change, as well as the role of legacy effects (e.g. reductions in plant growth, damage to the plant&#8217;s hydraulic transport system), that drive multi-timescale feedbacks. In particular, the role … Show more
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