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Negative impacts of high temperatures on growth of black spruce forests intensify with the anticipated climate warming

机译:预期的气候变暖加剧了高温对黑云杉林生长的负面影响

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An increasing number of studies conclude that water limitations and heat stress may hinder the capacity of black spruce (Picea mariana (Mill.) B.S.P.) trees, a dominant species of Canada's boreal forests, to grow and assimilate atmospheric carbon. However, there is currently no scientific consensus on the future of these forests over the next century in the context of widespread climate warming. The large spatial extent of black spruce forests across the Canadian boreal forest and associated variability in climate, demography, and site conditions pose challenges for projecting future climate change responses. Here we provide an evaluation of the impacts of climate warming and drying, as well as increasing [CO2], on the aboveground productivity of black spruce forests across Canada south of 60 degrees N for the period 1971 to 2100. We use a new extensive network of tree-ring data obtained from Canada's National Forest Inventory, spatially explicit simulations of net primary productivity (NPP) and its drivers, and multivariate statistical modeling. We found that soil water availability is a significant driver of black spruce interannual variability in productivity across broad areas of the western to eastern Canadian boreal forest. Interannual variability in productivity was also found to be driven by autotrophic respiration in the warmest regions. In most regions, the impacts of soil water availability and respiration on interannual variability in productivity occurred during the phase of carbohydrate accumulation the year preceding tree-ring formation. Results from projections suggest an increase in the importance of soil water availability and respiration as limiting factors on NPP over the next century due to warming, but this response may vary to the extent that other factors such as carbon dioxide fertilization, and respiration acclimation to high temperature, contribute to dampening these limitations.
机译:越来越多的研究得出结论,水的限制和热应激可能会阻碍黑云杉(Picea mariana(Mill。)B.S.P.)树木的生长和吸收大气碳的能力。黑云杉是加拿大北方森林的主要树种。然而,在广泛的气候变暖的背景下,目前尚无科学共识,就这些森林在下个世纪的未来进行探讨。整个加拿大北方森林中的黑云杉林的空间范围很大,而且气候,人口和地点条件的相关变化也给预测未来的气候变化对策构成了挑战。在这里,我们提供了1971年至2100年期间气候变暖和干燥以及[CO2]升高对加拿大北纬60度以南的加拿大黑云杉林地上生产力的影响的评估。我们使用新的广泛网络从加拿大国家森林清单获得的树木年轮数据,净初级生产力(NPP)及其驱动因素的空间显式模拟以及多元统计模型。我们发现,在加拿大西部至东部寒带林的大片地区,土壤水供应量是造成黑云杉年生产力变化的重要驱动力。生产力的年际变化也被最温暖地区的自养呼吸所驱动。在大多数地区,土壤水可利用性和呼吸作用对生产力的年际变化的影响发生在树木年轮形成前一年的碳水化合物积累阶段。预测结果表明,由于变暖,土壤水的可用性和呼吸作为下一个世纪NPP的限制因素的重要性增加,但是这种反应的程度可能会有所不同,例如二氧化碳施肥和呼吸适应达到高水平。温度,有助于减轻这些限制。

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