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Stream Physical Characteristics Impact Habitat Quality for Pacific Salmon in Two Temperate Coastal Watersheds

机译:溪流物理特征影响两个温带沿海流域太平洋鲑鱼的生境质量

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摘要

Climate warming is likely to cause both indirect and direct impacts on the biophysical properties of stream ecosystems especially in regions that support societally important fish species such as Pacific salmon. We studied the seasonal variability and interaction between stream temperature and DO in a low-gradient, forested stream and a glacial-fed stream in coastal southeast Alaska to assess how these key physical parameters impact freshwater habitat quality for salmon. We also use multiple regression analysis to evaluate how discharge and air temperature influence the seasonal patterns in stream temperature and DO. Mean daily stream temperature ranged from 1.1 to 16.4°C in non-glacial Peterson Creek but only 1.0 to 8.8°C in glacial-fed Cowee Creek, reflecting the strong moderating influence glacier meltwater had on stream temperature. Peterson Creek had mean daily DO concentrations ranging from 3.8 to 14.1 mg L−1 suggesting future climate changes could result in an even greater depletion in DO. Mean daily stream temperature strongly controlled mean daily DO in both Peterson (R2=0.82, P<0.01) and Cowee Creek (R2=0.93, P<0.01). However, DO in Peterson Creek was mildly related to stream temperature (R2=0.15, P<0.01) and strongly influenced by discharge (R2=0.46, P<0.01) on days when stream temperature exceeded 10°C. Moreover, Peterson Creek had DO values that were particularly low (<5.0 mg L−1) on days when discharge was low but also when spawning salmon were abundant. Our results demonstrate the complexity of stream temperature and DO regimes in coastal temperate watersheds and highlight the need for watershed managers to move towards multi-factor risk assessment of potential habitat quality for salmon rather than single factor assessments alone.
机译:气候变暖很可能对河流生态系统的生物物理特性造成间接和直接影响,特别是在那些支持具有社会重要意义的鱼类如太平洋鲑鱼的地区。我们研究了阿拉斯加东南沿海低梯度森林流和冰河中的水流温度和溶解氧的季节变化和相互作用,以评估这些关键的物理参数如何影响鲑鱼的淡水生境质量。我们还使用多元回归分析来评估排放量和气温如何影响溪流温度和溶解氧的季节性变化。在非冰川的彼得森河中,日平均河水温度在1.1至16.4°C之间,而在以冰川喂养的Cowee Creek中,日平均河水温度仅在1.0至8.8°C之间,这反映了冰川融水对河流温度的强烈调节作用。彼得森克里克(Peterson Creek)的每日平均溶解氧浓度范围为3.8至14.1 mg L -1 ,这表明未来的气候变化可能导致溶解氧的消耗更大。 Peterson(R 2 = 0.82,P <0.01)和Cowee Creek(R 2 = 0.93,P <0.01)的日平均河水温度均强烈控制了日均DO。然而,彼得森河中的溶解氧与河水温度有轻微的相关性(R 2 = 0.15,P <0.01),而受到排放的强烈影响(R 2 = 0.46,P <0.01)。 ),当水流温度超过10°C时。此外,在排放量低但产卵鲑鱼丰富的日子里,Peterson Creek的DO值特别低(<5.0 mg L -1 )。我们的结果表明,沿海温带流域的河流温度和溶解氧溶解度很复杂,并强调了流域管理者需要转向对鲑鱼的潜在栖息地质量进行多因素风险评估,而不是仅进行单因素评估。

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