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热带森林地区推断的干旱诱导植物分配变化及其对干旱遗留效应的影响。

Inferred drought-induced plant allocation shifts and their impact on drought legacy at a tropical forest site.

作者信息

Worden Matthew A, Famiglietti Caroline A, Levine Paul A, Ma Shuang, Bloom A Anthony, Bonal Damien, Stahl Clément, Konings Alexandra G

机构信息

Department of Earth System Science, Stanford University, Stanford, California, USA.

HydroSat, Washington, District of Columbia, USA.

出版信息

Glob Chang Biol. 2024 May;30(5):e17287. doi: 10.1111/gcb.17287.

Abstract

While droughts predominantly induce immediate reductions in plant carbon uptake, they can also exert long-lasting effects on carbon fluxes through associated changes in leaf area, soil carbon, etc. Among other mechanisms, shifts in carbon allocation due to water stress can contribute to the legacy effects of drought on carbon fluxes. However, the magnitude and impact of these allocation shifts on carbon fluxes and pools remain poorly understood. Using data from a wet tropical flux tower site in French Guiana, we demonstrate that drought-induced carbon allocation shifts can be reliably inferred by assimilating Net Biosphere Exchange (NBE) and other observations within the CARbon DAta MOdel fraMework. This model-data fusion system allows inference of optimized carbon and water cycle parameters and states from multiple observational data streams. We then examined how these inferred shifts affected the duration and magnitude of drought's impact on NBE during and after the extreme event. Compared to a static allocation scheme analogous to those typically implemented in land surface models, dynamic allocation reduced average carbon uptake during drought recovery by a factor of 2.8. Additionally, the dynamic model extended the average recovery time by 5 months. The inferred allocation shifts influenced the post-drought period by altering foliage and fine root pools, which in turn modulated gross primary productivity and heterotrophic respiration for up to a decade. These changes can create a bust-boom cycle where carbon uptake is enhanced some years after a drought, compared to what would have occurred under drought-free conditions. Overall, allocation shifts accounted for 65% [45%-75%] of drought legacy effects in modeled NBE. In summary, drought-induced carbon allocation shifts can play a substantial role in the enduring influence of drought on cumulative land-atmosphere CO exchanges and should be accounted for in ecosystem models.

摘要

虽然干旱主要导致植物碳吸收立即减少,但它们也会通过叶面积、土壤碳等相关变化对碳通量产生持久影响。在其他机制中,水分胁迫导致的碳分配变化可能会导致干旱对碳通量的遗留效应。然而,这些分配变化对碳通量和碳库的大小及影响仍知之甚少。利用法属圭亚那一个潮湿热带通量塔站点的数据,我们证明,通过在碳数据模型框架内同化净生物圈交换(NBE)和其他观测数据,可以可靠地推断干旱引起的碳分配变化。这个模型 - 数据融合系统允许从多个观测数据流推断优化的碳和水循环参数及状态。然后,我们研究了这些推断出的变化如何影响极端事件期间及之后干旱对NBE影响的持续时间和幅度。与陆地表面模型中通常采用的类似静态分配方案相比,动态分配使干旱恢复期间的平均碳吸收减少了2.8倍。此外,动态模型将平均恢复时间延长了5个月。推断出的分配变化通过改变叶片和细根碳库影响干旱后时期,进而在长达十年的时间里调节总初级生产力和异养呼吸。这些变化可能会形成一个兴衰循环,即与无干旱条件下相比,干旱几年后碳吸收会增强。总体而言,在模拟的NBE中,分配变化占干旱遗留效应的65%[45% - 75%]。总之,干旱引起的碳分配变化在干旱对陆地 - 大气累计CO交换的持久影响中可能起重要作用,应在生态系统模型中予以考虑。

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