Like other dryland regions around the world, the U.S. Southwest is on a steep trajectory towards a hotter and drier climate. Among the most conspicuous effects of this drying are large-scale vegetation transitions towards sparser systems and lower growth forms. Such structural transformations will have far-reaching consequences for ecosystem functioning and for the climate feedbacks of dryland vegetation. These feedbacks remain undervalued and understudied in a climate mitigation context, because drylands sequester less carbon per area compared to more mesic systems.
Tree-Ring Talk
