英文摘要: | Drought and heat-induced tree mortality is accelerating in many forest biomes as a consequence of a warming climate, resulting in a threat to global forests unlike any in recorded history1, 2, 3, 4, 5, 6, 7, 8, 9, 10, 11, 12. Forests store the majority of terrestrial carbon, thus their loss may have significant and sustained impacts on the global carbon cycle11, 12. We use a hydraulic corollary to Darcy’s law, a core principle of vascular plant physiology13, to predict characteristics of plants that will survive and die during drought under warmer future climates. Plants that are tall with isohydric stomatal regulation, low hydraulic conductance, and high leaf area are most likely to die from future drought stress. Thus, tall trees of old-growth forests are at the greatest risk of loss, which has ominous implications for terrestrial carbon storage. This application of Darcy’s law indicates today’s forests generally should be replaced by shorter and more xeric plants, owing to future warmer droughts and associated wildfires and pest attacks. The Darcy’s corollary also provides a simple, robust framework for informing forest management interventions needed to promote the survival of current forests. Given the robustness of Darcy’s law for predictions of vascular plant function, we conclude with high certainty that today’s forests are going to be subject to continued increases in mortality rates that will result in substantial reorganization of their structure and carbon storage.
Rates of tree mortality have risen substantially throughout much of North America in recent decades1, 2. Documentation of regional forest mortality events has increased globally3 in regions as disparate as Alaskan and Amazonian rainforests4, 5, from boreal forests of North America2 to semiarid forests of Southwestern USA6, Mediterranean Europe7 and Australia8. Forest loss often occurs rapidly whereas forest re-establishment and tree regrowth are much slower9, and in many cases post-mortality succession is dominated by smaller trees or shrubs and grasses that store less carbon (ref. 10; Fig. 1). The identified culprit is warming temperatures that, when superimposed on episodic periods of low precipitation, result in severe water deficits6. Given forecasts of continued rising temperatures and more extreme droughts globally11, 12, there are increasing risks of massive disruption of today’s forests during this century6, 10, 11, 12.
| http://www.nature.com/nclimate/journal/v5/n7/full/nclimate2641.html
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