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Terrestrial carbon balance in a drier world: the effects of water availability in southwestern North America

机译:干旱世界中的陆地碳平衡:北美西南部水资源的影响

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Global modeling efforts indicate semiarid regions dominate the increasing trend and interannual variation of net CO2 exchange with the atmosphere, mainly driven by water availability. Many semiarid regions are expected to undergo climatic drying, but the impacts on net CO2 exchange are poorly understood due to limited semiarid flux observations. Here we evaluated 121 site-years of annual eddy covariance measurements of net and gross CO2 exchange (photosynthesis and respiration), precipitation, and evapotranspiration (ET) in 21 semiarid North American ecosystems with an observed range of 100 - 1000mm in annual precipitation and records of 4-9years each. In addition to evaluating spatial relationships among CO2 and water fluxes across sites, we separately quantified site-level temporal relationships, representing sensitivity to interannual variation. Across the climatic and ecological gradient, photosynthesis showed a saturating spatial relationship to precipitation, whereas the photosynthesis-ET relationship was linear, suggesting ET was a better proxy for water available to drive CO2 exchanges after hydrologic losses. Both photosynthesis and respiration showed similar site-level sensitivity to interannual changes in ET among the 21 ecosystems. Furthermore, these temporal relationships were not different from the spatial relationships of long-term mean CO2 exchanges with climatic ET. Consequently, a hypothetical 100-mm change in ET, whether short term or long term, was predicted to alter net ecosystem production (NEP) by 64 gCm(-2)yr(-1). Most of the unexplained NEP variability was related to persistent, site-specific function, suggesting prioritization of research on slow-changing controls. Common temporal and spatial sensitivity to water availability increases our confidence that site-level responses to interannual weather can be extrapolated for prediction of CO2 exchanges over decadal and longer timescales relevant to societal response to climate change.
机译:全球模拟工作表明,半干旱地区主导着与大气净二氧化碳交换量的增长趋势和年际变化,这主要是由水的可利用性驱动的。预计许多半干旱地区将经历气候干燥,但是由于有限的半干旱通量观测结果,对净二氧化碳交换的影响了解得很少。在这里,我们评估了北美21个半干旱生态系统中净和总CO2交换(光合作用和呼吸作用),降水和蒸散(ET)的年度涡度协方差测量的121个站点-年,观测到的年降水量和记录范围为100-1000mm每个4-9年。除了评估跨站点的CO2和水通量之间的空间关系外,我们还分别量化了站点级别的时间关系,以表示对年际变化的敏感性。在整个气候和生态梯度上,光合作用显示出与降水的饱和空间关系,而光合作用与ET的关系则是线性的,这表明ET是水力流失后可用来驱动CO2交换的水的较好替代。光合作用和呼吸作用在21个生态系统中对ET的年际变化都显示出相似的位点敏感性。此外,这些时间关系与长期平均CO2与气候ET交换的空间关系没有区别。因此,预计无论短期还是长期,ET的假设100毫米变化都会使净生态系统产量(NEP)降低64 gCm(-2)yr(-1)。大部分无法解释的NEP变异性与持续的,特定于位点的功能有关,这表明优先研究缓慢变化的对照。对水的普遍时空敏感性提高了我们的信心,即可以推断出年际天气的场地水平响应,以预测与气候变化的社会响应相关的十年和更长的时间范围内的二氧化碳交换。

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