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首页> 外文期刊>Global change biology >The threat to coral reefs from more intense cyclones under climate change
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The threat to coral reefs from more intense cyclones under climate change

机译:气候变化下更强烈的气旋对珊瑚礁的威胁

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Ocean warming under climate change threatens coral reefs directly, through fatal heat stress to corals and indirectly, by boosting the energy of cyclones that cause coral destruction and loss of associated organisms. Although cyclone frequency is unlikely to rise, cyclone intensity is predicted to increase globally, causing more frequent occurrences of the most destructive cyclones with potentially severe consequences for coral reef ecosystems. While increasing heat stress is considered a pervasive risk to coral reefs, quantitative estimates of threats from cyclone intensification are lacking due to limited data on cyclone impacts to inform projections. Here, using extensive data from Australia's Great Barrier Reef (GBR), we show that increases in cyclone intensity predicted for this century are sufficient to greatly accelerate coral reef degradation. Coral losses on the outer GBR were small, localized and offset by gains on undisturbed reefs for more than a decade, despite numerous cyclones and periods of record heat stress, until three unusually intense cyclones over 5 years drove coral cover to record lows over > 1500 km. Ecological damage was particularly severe in the central-southern region where 68 of coral cover was destroyed over > 1000 km, forcing record declines in the species richness and abundance of associated fish communities, with many local extirpations. Four years later, recovery of average coral cover was relatively slow and there were further declines in fish species richness and abundance. Slow recovery of community diversity appears likely from such a degraded starting point. Highly unusual characteristics of two of the cyclones, aside from high intensity, inflated the extent of severe ecological damage that would more typically have occurred over 100s of km. Modelling published predictions of future cyclone activity, the likelihood of more intense cyclones within time frames of coral recovery by mid-century poses a global threat to coral reefs and dependent societies.
机译:气候变化下的海洋变暖通过对珊瑚的致命热应激直接威胁珊瑚礁,并通过增加导致珊瑚破坏和相关生物丧失的气旋的能量间接威胁珊瑚礁。尽管气旋频率不太可能上升,但预计全球气旋强度将增加,导致更具破坏性的气旋更频繁地发生,对珊瑚礁生态系统造成潜在严重后果。虽然日益增加的热应激被认为是对珊瑚礁的普遍风险,但由于关于气旋影响的数据有限,无法为预测提供信息,因此缺乏对气旋加剧威胁的定量估计。在这里,利用来自澳大利亚大堡礁(GBR)的大量数据,我们表明,本世纪预测的气旋强度增加足以大大加速珊瑚礁退化。尽管有无数次飓风和创纪录的热应激时期,但十多年来,外GBR的珊瑚损失很小,局部性并被未受干扰的珊瑚礁的增加所抵消,直到5年内三次异常强烈的气旋将珊瑚覆盖率推至1500公里>创纪录的低点。中南部地区的生态破坏尤为严重,在1000公里>,68%的珊瑚覆盖被破坏,迫使相关鱼类群落的物种丰富度和丰度创纪录下降,许多地方灭绝。四年后,平均珊瑚覆盖率的恢复相对缓慢,鱼类物种的丰富度和丰度进一步下降。从这样一个退化的起点开始,社区多样性的缓慢恢复似乎是可能的。除了高强度之外,其中两个气旋的极不寻常的特征夸大了严重生态破坏的程度,这种破坏通常发生在100多公里的范围内。根据对未来气旋活动的已发表预测进行建模,到本世纪中叶,在珊瑚恢复的时间范围内出现更强烈的气旋的可能性对珊瑚礁和依赖社会构成了全球威胁。

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