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Gross primary production responses to warming, elevated CO2, and irrigation:quantifying the drivers of ecosystem physiology in a semiarid grassland

机译:初级生产总值对变暖,CO2升高和灌溉的反应:量化半干旱草原生态系统生理的驱动力

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摘要

Determining whether the terrestrial biosphere will be a source or sink of carbon (C) under a future climate of elevated CO2 (eCO2) and warming requires accurate quantification of gross primary production (GPP), the largest flux of C in the global C cycle. We evaluated six years (2007-2012) of flux-derived GPP data (~2500 values) from the Prairie Heating and CO2 Enrichment (PHACE) experiment, situated in a mixed prairie grassland in Wyoming, USA. The GPP data were used to calibrate a light response model whose basic formulation has been successfully used in a variety of ecosystems. The model, however, was extended to allow for variable maximum photosynthetic rate (Amax) and light-use efficiency (Q) by modeling these terms as functions of time varying driving variables (soil water content, air temperature, vapor pressure deficit, vegetation greenness, nitrogen) at current and antecedent (past) time scales. The model fit the observed GPP well (R2 = 0.79), which was confirmed by other model performance checks (deviance information criterion and posterior predictive loss) that compared different variants of the model (e.g., with and without antecedent effects). Stimulation of cumulative six-year GPP by warming (29%, P=0.02) and eCO2 (26%, P=0.07) was primarily driven by enhanced C uptake during spring (129%, P=0.001) and fall (124%, P=0.001), respectively. These enhancements were consistent across each year, suggesting mechanisms for extending the growing season. Antecedent air temperature (Tairant) and vapor pressure deficit (VPDant) effects on Amax were the most significant predictors of temporal variability in GPP among most treatments. The importance of VPDant suggests that atmospheric drought plays an important role for predicting GPP under current and future climate. Given the limited research supporting the role of VPDant in this context, we highlight the need for experimental studies to identify the mechanisms underlying such antecedent effects.
机译:在未来二氧化碳浓度升高(eCO2)和变暖的未来气候下,确定陆地生物圈将是碳(C)的源还是碳汇,需要精确量化初级总产值(GPP),这是全球C循环中最大的C通量。我们通过位于美国怀俄明州大草原混合草原的草原加热和二氧化碳富集(PHACE)实验评估了六年(2007-2012年)的通量派生GPP数据(〜2500值)。 GPP数据用于校准光响应模型,其基本公式已成功用于各种生态系统中。然而,通过将这些术语建模为随时间变化的驱动变量(土壤含水量,空气温度,蒸气压赤字,植被绿度)的函数,该模型被扩展为允许可变的最大光合速率(Amax)和光利用效率(Q)。 ,氮)在当前和以前(过去)的时间尺度上。该模型非常符合观察到的GPP(R2 = 0.79),这已通过其他模型性能检查(偏离信息标准和后验预测损失)得到了证实,这些检查比较了模型的不同变体(例如,有或没有先例效应)。春季(129%,P = 0.001)和秋季(124%,124%)的碳吸收增加主要是通过变暖(29%,P = 0.02)和eCO2(26%,P = 0.07)来刺激累积的六年GPP。 P = 0.001)。这些增强在每一年都是一致的,提示了延长生长期的机制。在大多数治疗中,前期气温(Tairant)和蒸气压赤字(VPDant)对Amax的影响是GPP时间变异性的最重要预测指标。 VPDant的重要性表明,大气干旱对于预测当前和未来气候下的GPP起着重要作用。鉴于支持VPDant在此背景下发挥作用的研究有限,我们强调需要进行实验研究来确定这种先发效应的潜在机制。

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