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Trade-offs between global warming and day length on the start of the carbon uptake period in seasonally cold ecosystems

机译:在季节性寒冷的生态系统中在碳吸收期开始时全球变暖与日长之间的权衡

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摘要

[1] It is well established that warming leads to longer growing seasons in seasonally cold ecosystems. Whether this goes along with an increase in the net ecosystem carbon dioxide (CO2) uptake is much more controversial. We studied the effects of warming on the start of the carbon uptake period (CUP) of three mountain grasslands situated along an elevational gradient in the Alps. To this end, we used a simple empirical model of the net ecosystem CO2 exchange, calibrated, and forced with multiyear empirical data from each site. We show that reductions in the quantity and duration of daylight associated with earlier snowmelts were responsible for diminishing returns, in terms of carbon gain, from longer growing seasons caused by reductions in daytime photosynthetic uptake and increases in nighttime losses of CO2. This effect was less pronounced at high, compared to low, elevations, where the start of the CUP occurred closer to the summer solstice when changes in day length and incident radiation are minimal.
机译:[1]众所周知,在季节性寒冷的生态系统中,变暖导致更长的生长季节。这是否与生态系统净二氧化碳(CO2)吸收量的增加同时引起争议。我们研究了变暖对沿阿尔卑斯山海拔梯度分布的三个高山草原碳吸收期(CUP)的影响。为此,我们使用了一个简单的生态系统净二氧化碳交换的经验模型,并根据每个站点的多年经验数据进行了校准和强制。我们发现,与早期融雪有关的日光数量和持续时间的减少是造成白天光合吸收减少和夜间CO2损失增加导致生长季节延长的收益减少(就碳增加而言)的原因。与高海拔相比,这种影响在低海拔处不那么明显,因为当日长和入射辐射的变化最小时,CUP的开始发生在夏至附近。

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