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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. Marine ecosystem drivers that contribute to stressing ecosystems - including warming, acidification, deoxygenation and perturbations to biological productivity - can co-occur in space and time, but detecting their trends is complicated by the presence of noise associated with natural variability in the climate system. Here we use large initial-condition ensemble simulations with an Earth system model under a historical/RCP8.5 (representative concentration pathway 8.5) scenario over 1950-2100 to consider emergence characteristics for the four individual and combined drivers. Using a 1-standard-deviation (67% confidence) threshold of signal to noise to define emergence with a 30-year trend window, we show that ocean acidification emerges much earlier than other drivers, namely during the 20th century over most of the global ocean. For biological productivity, the anthropogenic signal does not emerge from the noise over most of the global ocean before the end of the 21st century. The early emergence pattern for sea surface temperature in low latitudes is reversed from that of subsurface oxygen inventories, where emergence occurs earlier in the Southern Ocean. For the combined multiple-driver field, 41% of the global ocean exhibits emergence for the 2005-2014 period, and 63% for the 2075-2084 period. The combined multiple-driver field reveals emergence patterns by the end of this century that are relatively high over much of the Southern Ocean, North Pacific, and Atlantic, but relatively low over the tropics and the South Pacific. For the case of two drivers, the tropics including habitats of coral reefs emerges earliest, with this driven by the joint effects of acidification and warming. It is precisely in the regions with pronounced emergence characteristics where marine ecosystems may be expected to be pushed outside of their comfort zone determined by the degree of natural background variability to which they are adapted. The results underscore the importance of sustained multi-decadal observing systems for monitoring multiple ecosystems drivers.
机译:人为改变给海洋生态系统带来的压力越来越大。造成气候变化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所带来的噪声的存在,检测其趋势变得复杂。在这里,我们在1950-2100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程序的出现特征。使用信噪比的1标准偏差(置信度为67%)阈值来定义30年趋势窗口的出现,我们表明,海洋酸化的出现要早于其他驱动因素,即在20世纪全球大部分地区海洋。对于生物生产力而言,在21世纪末之前,全球大部分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气清单的发生方式相反,后者在南部海洋中出现较早。对于多驱动器组合领域,2005-2014年期间出现了全球海洋的41%,2075-2084年期间出现了63%。到本世纪末,由多个驱动因素组成的联合场揭示了涌现模式,在南大洋,北太平洋和大西洋的大部分地区相对较高,而在热带和南太平洋则相对较低。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。恰恰在出现显着特征的地区,海洋生态系统可能会被推到其舒适区之外,而舒适区则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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