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Climate change impacts on streamflow extremes and summertime stream temperature and their possible consequences for freshwater salmon habitat in Washington State

机译:气候变化对河流极端流量和夏季河流温度的影响及其对华盛顿州淡水鲑鱼栖息地的可能影响

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This study evaluates the sensitivity of Washington State's freshwater habitat of Pacific Salmon (Oncorhynchus spp.) to climate change. Our analysis focuses on summertime stream temperatures, seasonal low flows, and changes in peak and base flows because these physical factors are likely to be key pressure points for many of Washington's salmon populations. Weekly summertime water temperatures and extreme daily high and low streamflows are evaluated under multimodel composites for A1B and B1 greenhouse gas emissions scenarios. Simulations predict rising water temperatures will thermally stress salmon throughout Washington's watersheds, becoming increasingly severe later in the twenty-first century. Streamflow simulations predict that basins strongly influenced by transient runoff (a mix of direct runoff from cool-season rainfall and springtime snowmelt) are most sensitive to climate change. By the 2080s, hydrologic simulations predict a complete loss of Washington's snowmelt dominant basins, and only about ten transient basins remaining in the north Cascades. Historically transient runoff watersheds will shift towards rainfall dominant behavior, undergoing more severe summer low flow periods and more frequent days with intense winter flooding. While cool-season stream temperature changes and impacts on salmon are not assessed in this study, it is possible that climate-induced warming in winter and spring will benefit parts of the freshwater life-cycle of some salmon populations enough to increase their reproductive success (or overall fitness). However, the combined effects of warming summertime stream temperatures and altered streamflows will likely reduce the reproductive success for many Washington salmon populations, with impacts varying for different life history-types and watershed-types. Diminishing streamflows and higher stream temperatures in summer will be stressful for stream-type salmon populations that have freshwater rearing periods in summer. Increased winter flooding in transient runoff watersheds will likely reduce the egg-to-fry survival rates for ocean-type and stream-type salmon.
机译:这项研究评估了华盛顿州太平洋鲑鱼(Oncorhynchus spp。)的淡水生境对气候变化的敏感性。我们的分析重点是夏季河水温度,季节性低流量以及高峰流量和基本流量的变化,因为这些物理因素可能是华盛顿许多鲑鱼种群的关键压力点。在A1B和B1温室气体排放情景的多模型复合材料下,评估了夏季夏季的水温和极端的每日高低流量。模拟预测,升高的水温将对整个华盛顿流域的鲑鱼造成热应力,在二十一世纪后期将变得越来越严重。流量模拟预测,受瞬态径流(冷季降雨和春季融雪的直接径流的混合)强烈影响的盆地对气候变化最敏感。到2080年代,水文模拟预测华盛顿的融雪占主导地位的盆地将完全消失,而北部喀斯喀特山脉仅剩下约十个过渡盆地。从历史上看,短暂的径流集水区将转向以降雨为主的行为,夏季将经历更严重的低流量期,而冬季则将出现频繁的洪灾。尽管本研究未评估冷季河流温度变化及其对鲑鱼的影响,但冬季和春季气候引起的变暖可能会使部分鲑鱼种群的淡水生命周期的一部分受益,足以增加其繁殖成功率(或整体适合度)。但是,夏季河水温度升高和河水流量变化的综合影响可能会降低许多华盛顿鲑鱼种群的繁殖成功率,其影响因生活史类型和流域类型而异。夏季水流减少和溪流温度升高,将对夏季淡水养殖期的溪流型鲑鱼种群造成压力。短暂径流集水区冬季洪水的增加可能会降低海洋型和溪流型鲑鱼卵到鱼的成活率。

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