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Emergence of multiple ocean ecosystem drivers in a large ensemble suite with an Earth system model

机译:具有地球系统模型的大型整体套件中多个海洋生态系统驱动程序的出现

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Marine ecosystems are increasingly stressed by human-induced changes. Marineecosystem drivers that contribute to stressing ecosystems – includingwarming, acidification, deoxygenation and perturbations to biologicalproductivity – can co-occur in space and time, but detecting their trends iscomplicated by the presence of noise associated with natural variability inthe climate system. Here we use large initial-condition ensemble simulationswith an Earth system model under a historical/RCP8.5 (representativeconcentration pathway 8.5) scenario over 1950–2100 to consider emergencecharacteristics for the four individual and combined drivers. Using a1-standard-deviation (67% confidence) threshold of signal to noise todefine emergence with a 30-year trend window, we show that oceanacidification emerges much earlier than other drivers, namely during the20th century over most of the global ocean. For biological productivity, theanthropogenic signal does not emerge from the noise over most of the globalocean before the end of the 21st century. The early emergence pattern for seasurface temperature in low latitudes is reversed from that of subsurfaceoxygen inventories, where emergence occurs earlier in the Southern Ocean. Forthe combined multiple-driver field, 41% of the global ocean exhibitsemergence for the 2005–2014 period, and 63% for the 2075–2084 period.The combined multiple-driver field reveals emergence patterns by the end ofthis century that are relatively high over much of the Southern Ocean, NorthPacific, and Atlantic, but relatively low over the tropics and the SouthPacific. For the case of two drivers, the tropics including habitats of coralreefs emerges earliest, with this driven by the joint effects ofacidification and warming. It is precisely in the regions with pronouncedemergence characteristics where marine ecosystems may be expected to bepushed outside of their comfort zone determined by the degree of naturalbackground variability to which they are adapted. The results underscore theimportance of sustained multi-decadal observing systems for monitoringmultiple ecosystems drivers.
机译:人为改变给海洋生态系统带来的压力越来越大。造成生态系统压力的海洋生态系统驱动因素(包括变暖,酸化,脱氧和对生物生产力的扰动)可以在空间和时间上同时发生,但是由于气候系统中自然变化带来的噪声的存在,检测其趋势变得复杂。在这里,我们在1950年至2100年的历史/RCP8.5(代表浓度路径8.5)方案下,使用带有地球系统模型的大型初始条件总体模拟,来考虑四个单独和组合驱动因素的出现特征。使用信噪比的a1-标准偏差(置信度为67%)阈值定义30年趋势窗口的出现,我们表明,海洋酸化的出现比其他驱动因素要早得多,即在20世纪全球大部分海洋中。对于生物生产力,在21世纪末之前,全球大多数海洋的噪声中都不会出现人为信号。低纬度地区海表温度的早期出现方式与地下氧清单相反,后者在南部大洋中出现较早。对于多驱动器组合场,2005-2014年期间全球海洋出现了41%,而2075-2084年期间则出现了63%。多驱动器合并后的区域显示了本世纪末相对较高的出现模式。南大洋,北太平洋和大西洋的大部分地区,但在热带和南太平洋相对较低。对于两个驱动器而言,包括珊瑚礁栖息地在内的热带地区最早出现,这是由酸化和变暖的共同作用驱动的。恰恰是在具有明显退化特征的区域中,海洋生态系统可能会在其舒适带之外被推翻,这取决于它们所适应的自然本底变化程度。结果强调了持续的多年代观测系统对监测多种生态系统驱动因素的重要性。

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