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Climate-driven trends and ecological implications of event-scale upwelling in the California Current System

机译:气候驱动趋势和加利福尼亚现行系统中事件规模上升的生态影响

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摘要

Eastern boundary current systems are among the most productive and lucrative ecosystems on Earth because they benefit from upwelling currents. Upwelling currents subsidize the base of the coastal food web by bringing deep, cold and nutrient-rich water to the surface. As upwelling is driven by large-scale atmospheric patterns, global climate change has the potential to affect a wide range of significant ecological processes through changes in water chemistry, water temperature, and the transport processes that influence species dispersal and recruitment. We examined long-term trends in the frequency, duration, and strength of continuous upwelling events for the Oregon and California regions of the California Current System in the eastern Pacific Ocean. We then associated event-scale upwelling with up to 21 similar to years of barnacle and mussel recruitment, and water temperature data measured at rocky intertidal field sites along the Oregon coast. Our analyses suggest that upwelling events are changing in ways that are consistent with climate change predictions: upwelling events are becoming less frequent, stronger, and longer in duration. In addition, upwelling events have a quasi-instantaneous and cumulative effect on rocky intertidal water temperatures, with longer events leading to colder temperatures. Longer, more persistent upwelling events were negatively associated with barnacle recruitment but positively associated with mussel recruitment. However, since barnacles facilitate mussel recruitment by providing attachment sites, increased upwelling persistence could have indirect negative impacts on mussel populations. Overall, our results indicate that changes in coastal upwelling that are consistent with climate change predictions are altering the tempo and the mode of environmental forcing in near-shore ecosystems, with potentially severe and discontinuous ramifications for ecosystem structure and functioning.
机译:东部边界洋流系统是地球上生产力最高,利润最高的生态系统之一,因为它们受益于上升流。上升流通过将深水,冷水和营养丰富的水带到地表来补贴沿海食物网的基础。由于上升流是由大规模大气模式驱动的,因此全球气候变化有可能通过水化学,水温以及影响物种扩散和吸收的运输过程的变化,影响广泛的重要生态过程。我们研究了东太平洋加利福尼亚洋流系统的俄勒冈州和加利福尼亚州地区持续上升事件的频率,持续时间和强度的长期趋势。然后,我们将事件规模的上升与多达21年的藤壶和贻贝募集相结合,并在俄勒冈州海岸沿岸的潮间带岩石现场测得的水温数据。我们的分析表明,上升流事件的变化方式与气候变化预测相一致:上升流事件的频率降低,强度越来越大,持续时间也越来越长。此外,上升流事件对潮间带岩石水温具有近似瞬时和累积的影响,较长的事件导致温度降低。更长,更持久的上升事件与藤壶的募集负相关,而与贻贝的募集正相关。但是,由于藤壶通过提供附着点来促进贻贝的募集,因此上升流的持续性可能对贻贝种群产生间接的负面影响。总体而言,我们的结果表明,与气候变化预测相一致的沿海上升流变化正在改变近岸生态系统中环境强迫的速度和方式,对生态系统的结构和功能可能产生严重的和不连续的影响。

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