Plant profit maximization improves predictions of European forest responses to drought

被引:70
|
作者
Sabot, Manon E. B. [1 ]
De Kauwe, Martin G. [1 ,2 ]
Pitman, Andy J. [1 ]
Medlyn, Belinda E. [3 ]
Verhoef, Anne [4 ]
Ukkola, Anna M. [5 ]
Abramowitz, Gab [1 ]
机构
[1] Univ New South Wales, ARC Ctr Excellence Climate Extremes & Climate Cha, Sydney, NSW 2052, Australia
[2] Univ New South Wales, Evolut & Ecol Res Ctr, Sydney, NSW 2052, Australia
[3] Western Sydney Univ, Hawkesbury Inst Environm, Locked Bag 1797, Penrith, NSW 2751, Australia
[4] Univ Reading, Dept Geog & Environm Sci, POB 227, Reading RG6 6AB, Berks, England
[5] Australian Natl Univ, ARC Ctr Excellence Climate Extremes & Res, Sch Earth Sci, Canberra, ACT 0200, Australia
基金
澳大利亚研究理事会; 英国自然环境研究理事会;
关键词
canopy gas exchange; hydraulic trait adjustments to climate; land surface models; plant optimality; plant profit maximization; plant trait coordination; vegetation drought responses; STOMATAL CONDUCTANCE; HYDRAULIC TRAITS; WATER-STRESS; ECOLOGICAL SIGNIFICANCE; CO2; ASSIMILATION; SOIL-WATER; MODEL; RESPIRATION; TRANSPIRATION; ACCLIMATION;
D O I
10.1111/nph.16376
中图分类号
Q94 [植物学];
学科分类号
071001 ;
摘要
Knowledge of how water stress impacts the carbon and water cycles is a key uncertainty in terrestrial biosphere models. We tested a new profit maximization model, where photosynthetic uptake of CO2 is optimally traded against plant hydraulic function, as an alternative to the empirical functions commonly used in models to regulate gas exchange during periods of water stress. We conducted a multi-site evaluation of this model at the ecosystem scale, before and during major droughts in Europe. Additionally, we asked whether the maximum hydraulic conductance in the soil-plant continuum k(max) (a key model parameter which is not commonly measured) could be predicted from long-term site climate. Compared with a control model with an empirical soil moisture function, the profit maximization model improved the simulation of evapotranspiration during the growing season, reducing the normalized mean square error by c. 63%, across mesic and xeric sites. We also showed that k(max) could be estimated from long-term climate, with improvements in the simulation of evapotranspiration at eight out of the 10 forest sites during drought. Although the generalization of this approach is contingent upon determining k(max), it presents a mechanistic trait-based alternative to regulate canopy gas exchange in global models.
引用
收藏
页码:1638 / 1655
页数:18
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