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首页> 外文期刊>Global change biology >Modelling the future hydroclimatology of the lower Fraser River and its impacts on the spawning migration survival of sockeye salmon
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Modelling the future hydroclimatology of the lower Fraser River and its impacts on the spawning migration survival of sockeye salmon

机译:模拟弗雷泽河下游的未来水文气候学及其对红鲑鲑的产卵迁徙生存的影响

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Short episodic high temperature events can be lethal for migrating adult Pacific salmon (Oncorhynchus spp.). We downscaled temperatures for the Fraser River, British Columbia to evaluate the impact of climate warming on the frequency of exceeding thermal thresholds associated with salmon migratory success. Alarmingly, a modest 1.0 degrees C increase in average summer water temperature over 100 years (1981-2000 to 2081-2100) tripled the number of days per year exceeding critical salmonid thermal thresholds (i.e. 19.0 degrees C). Refined thresholds for two populations (Gates Creek and Weaver Creek) of sockeye salmon (Oncorhynchus nerka) were defined using physiological constraint models based on aerobic scope. While extreme temperatures leading to complete aerobic collapse remained unlikely under our warming scenario, both populations were increasingly forced to migrate upriver at reduced levels of aerobic performance (e.g. in 80% of future simulations, >= 90% of salmon encountered temperatures exceeding population-specific thermal optima for maximum aerobic scope; T-opt=16.3 degrees C for Gates Creek and T-opt=14.5 degrees C for Weaver Creek). Assuming recent changes to river entry timing persist, we also predicted dramatic increases in the probability of freshwater mortality for Weaver Creek salmon due to reductions in aerobic, and general physiological, performance (e.g. in 42% of future simulations >= 50% of Weaver Creek fish exceeded temperature thresholds associated with 0-60% of maximum aerobic scope). Potential for adaptation via directional selection on run-timing was more evident for the Weaver Creek population. Early entry Weaver Creek fish experienced 25% (range: 15-31%) more suboptimal temperatures than late entrants, compared with an 8% difference (range: 0-17%) between early and late Gates Creek fish. Our results emphasize the need to consider daily temperature variability in association with population-specific differences in behaviour and physiological constraints when forecasting impacts of climate change on migratory survival of aquatic species.
机译:短暂的高温事件可能会使成年太平洋鲑鱼(Oncorhynchus spp。)迁徙。我们降低了不列颠哥伦比亚省弗雷泽河的温度,以评估气候变暖对超过与鲑鱼迁徙成功相关的热阈值频率的影响。令人震惊的是,超过100年(1981-2000年至2081-2100年)的夏季平均水温仅温和地升高了1.0摄氏度,超过了严格的鲑鱼热阈值(即19.0摄氏度),每年的天数增加了两倍。使用基于有氧范围的生理约束模型,定义了红鲑(Oncorhynchus nerka)的两个种群(Gates Creek和Weaver Creek)的精确阈值。尽管在我们的变暖情况下,极端温度不会导致有氧运动完全崩溃,但是两个种群都越来越多地被迫在有氧运动水平降低的情况下向上游迁移(例如,在80%的未来模拟中,> = 90%的鲑鱼遇到的温度超过了特定种群的温度最大有氧范围的最佳温度;盖茨溪为T-opt = 16.3摄氏度,韦弗溪为T-opt = 14.5摄氏度)。假设河流进入时间的最新变化持续存在,我们还预测由于有氧和一般生理性能的降低,Weaver Creek鲑鱼的淡水死亡概率将急剧增加(例如,在未来的模拟中有42%> Weaver Creek的50%以上)鱼超过了与最大有氧范围的0-60%相关的温度阈值。对于Weaver Creek种群,通过运行时机上的方向选择进行适应的潜力更加明显。早进Weaver Creek鱼比晚进者经历的次优温度高25%(范围:15-31%),而盖茨溪早与晚鱼之间的差异为8%(范围:0-17%)。我们的研究结果强调了在预测气候变化对水生物种迁徙生存的影响时,需要考虑日常温度变化与行为和生理限制的特定人群差异。

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