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Physical forcing and the dynamics of the pelagic ecosystem in the eastern tropical Pacific: simulations with ENSO-scale and global-warming climate drivers

机译:东部热带太平洋的物理强迫和中上层生态系统的动力学:使用ENSO尺度和全球变暖气候驱动因素的模拟

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摘要

We used a model of the pelagic ecosystem in the eastern tropical Pacific Ocean to explore how climate variation at El Nino - Southern Oscillation (ENSO) scales might affect animals at middle and upper trophic levels. We developed two physical-forcing scenarios: (1) physical effects on phytoplankton biomass and (2) simultaneous physical effects on phytoplankton biomass and predator recruitment. We simulated the effects of climate-anomaly pulses, climate cycles, and global warming. Pulses caused oscillations to propagate through the ecosystem; cycles affected the shapes of these oscillations; and warming caused trends. We concluded that biomass trajectories of single populations at middle and upper trophic levels cannot be used to detect bottom-up effects, that direct physical effects on predator recruitment can be the dominant source of interannual variability in pelagic ecosystems, that such direct effects may dampen top-down control by fisheries, and that predictions about the effects of climate change may be misleading if fishing mortality is not considered. Predictions from ecosystem models are sensitive to the relative strengths of indirect and direct physical effects on middle and upper trophic levels.
机译:我们使用了东部热带太平洋中上层生态系统的模型来研究厄尔尼诺-南方涛动(ENSO)尺度的气候变化如何影响中高层营养水平的动物。我们开发了两种物理强迫方案:(1)对浮游植物生物量的物理影响,以及(2)对浮游植物生物量和捕食者同时发生的物理影响。我们模拟了气候异常脉冲,气候周期和全球变暖的影响。脉冲导致振荡在整个生态系统中传播;周期影响了这些振荡的形状;和变暖导致趋势。我们得出的结论是,不能将中,高层营养水平的单个种群的生物量轨迹用于检测自下而上的影响,对捕食者募集的直接物理影响可能是中上层生态系统年际变化的主要来源,这种直接影响可能会抑制顶部如果不考虑捕捞死亡率,对渔业的控制权下降以及关于气候变化影响的预测可能会产生误导。生态系统模型的预测对中,高层营养水平的间接和直接物理影响的相对强度很敏感。

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