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Modeling Coral Bleaching Mitigation Potential of Water Vertical Translocation – An Analogue to Geoengineered Artificial Upwelling

机译:水垂直易位的珊瑚漂白缓解潜力 - 一种模拟到地衰老性人工升值

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Artificial upwelling (AU) is a novel geoengineering technology that brings seawater from the deep ocean to the surface. Within the context of global warming, AU techniques are proposed to reduce sea surface temperature at times of thermal stress around coral reefs. A computationally fast but coarse 3D Earth System model (3.6° longitude × 1.8° latitude) was used to investigate the environmental impacts of hypothetically implemented AU strategies in the Great Barrier Reef, South China Sea, and Hawaiian regions. While omitting the discussion on sub-grid hydrology, we simulated in our model a water translocation from either 130 or 550 m depth to sea surface at rates of 1 or 50 m3 s?1 as analogues to AU implementation. Under the Representative Concentration Pathway 8.5 emissions scenario from year 2020 on, the model predicted a prevention of coral bleaching until the year 2099 when AU was implemented, except under the least intense AU scenario (water from 130 m depth at 1 m3 s?1). Yet, intense AU implementation (water from 550 m depth at 50 m3 s-1) will likely have adverse effects on coral reefs by overcooling the surface water, altering salinity, decreasing calcium carbonate saturation, and considerably increasing nutrient levels. Our result suggests that if we utilize AU for mitigating coral bleaching during heat stress, AU implementation needs to be carefully designed with respect to AU’s location, depth, intensity and duration so that undesirable environmental effects are minimized. Following a proper installation and management procedure, however, AU has the potential to decelerate destructive bleaching events and buy corals more time to adjust to climate change.
机译:人工上升(AU)是一种新型地理工程技术,将海水从深海到表面带来。在全球变暖的背景下,提出了Au技术在珊瑚礁周围的热应力时减少海面温度。计算出快速但粗糙的3D地球系统模型(3.6°经度×1.8°纬度)用于调查假设实施的AU策略在大堡礁,南海和夏威夷地区的环境影响。虽然省略了对子网格水文的讨论,我们在我们的模型中模拟了从130或550米深度到海面的水易位,以1或50m 3 s的速率为1或50m 3 S?1作为类似AU实现的。在代表性浓度途径8.5年从2020年开始的排放情景下,该模型预测了预防珊瑚漂白,直到2099年,除了欧洲议会,除了在最小的AU场景中(130米深度为1 M3 S的水) 。然而,通过过冷却表面水,改变盐度,降低碳酸钙饱和度,并且大大增加碳酸钙饱和度,并且显着增加碳酸钙饱和度并显着增加碳酸钙饱和度并显着增加碳酸钙饱和度,迫使Au实施(550米深度为550米的水)可能对珊瑚礁产生不利影响。我们的结果表明,如果我们利用Au在热应激期间用于减轻珊瑚漂白,则需要在Au的位置,深度,强度和持续时间内仔细设计Au实现,使得不希望的环境影响最小化。然而,在适当的安装和管理程序之后,AU可能有可能减速破坏性的漂白事件,并更多地购买珊瑚时间来调整气候变化。

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