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High spatiotemporal variability of methane concentrations challenges estimates of emissions across vegetated coastal ecosystems

机译:甲烷浓度的高时空变化性对植被沿海生态系统的排放量估算提出了挑战

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摘要

Coastal methane (CH4) emissions dominate the global ocean CH4 budget and can offset the "blue carbon" storage capacity of vegetated coastal ecosystems. However, current estimates lack systematic, high-resolution, and long-term data from these intrinsically heterogeneous environments, making coastal budgets sensitive to statistical assumptions and uncertainties. Using continuous CH4 concentrations, delta C-13-CH4 values, and CH4 sea-air fluxes across four seasons in three globally pervasive coastal habitats, we show that the CH4 distribution is spatially patchy over meter-scales and highly variable in time. Areas with mixed vegetation, macroalgae, and their surrounding sediments exhibited a spatiotemporal variability of surface water CH4 concentrations ranging two orders of magnitude (i.e., 6-460 nM CH4) with habitat-specific seasonal and diurnal patterns. We observed (1) delta C-13-CH signatures that revealed habitat-specific CH4 production and consumption pathways, (2) daily peak concentration events that could change >100 within hours across all habitats, and (3) a high thermal sensitivity of the CH4 distribution signified by apparent activation energies of similar to 1 eV that drove seasonal changes. Bootstrapping simulations show that scaling the CH4 distribution from few samples involves large errors, and that similar to 50 concentration samples per day are needed to resolve the scale and drivers of the natural variability and improve the certainty of flux calculations by up to 70. Finally, we identify northern temperate coastal habitats with mixed vegetation and macroalgae as understudied but seasonally relevant atmospheric CH4 sources (i.e., releasing >= 100 mu mol CH4 m(-2) day(-1) in summer). Due to the large spatial and temporal heterogeneity of coastal environments, high-resolution measurements will improve the reliability of CH4 estimates and confine the habitat-specific contribution to regional and global CH4 budgets.
机译:沿海甲烷 (CH4) 排放在全球海洋 CH4 预算中占主导地位,可以抵消植被沿海生态系统的“蓝碳”储存能力。然而,目前的估计缺乏来自这些本质异质环境的系统、高分辨率和长期数据,使沿海预算对统计假设和不确定性很敏感。使用连续的CH4浓度,delta C-13-CH4值和CH4海气通量,在三个全球普遍的沿海栖息地的四个季节中,我们发现CH4的分布在米尺度上是空间斑块的,并且在时间上变化很大。植被、大型藻类及其周围沉积物混合的区域地表水CH4浓度的时空变化范围为两个数量级(即6-460 nM CH4),具有生境特定的季节和昼夜模式。我们观察到 (1) delta C-13-CH 特征揭示了栖息地特异性 CH4 的生产和消费途径,(2) 所有栖息地的每日峰值浓度事件可能在数小时内变化 >100%,以及 (3) CH4 分布的高热敏感性,其标志是类似于 1 eV 的表观活化能驱动季节性变化。自举模拟表明,从少量样品中缩放CH4分布涉及较大的误差,并且需要每天50个浓度样品来解析自然变异性的尺度和驱动因素,并将通量计算的确定性提高多达70%。最后,我们将具有混合植被和大型藻类的北温带沿海生境确定为未被充分研究但与季节性相关的大气 CH4 来源(即,夏季释放 >= 100 μ mol CH4 m(-2) 天 (-1))。由于沿海环境在空间和时间上具有很大的异质性,高分辨率测量将提高CH4估计值的可靠性,并限制特定生境对区域和全球CH4预算的贡献。

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