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考虑地下水对溪流鱼类热生境响应气候变化的影响。

Accounting for groundwater in stream fish thermal habitat responses to climate change.

出版信息

Ecol Appl. 2015 Jul;25(5):1397-419. doi: 10.1890/14-1354.1.

Abstract

Forecasting climate change effects on aquatic fauna and their habitat requires an understanding of how water temperature responds to changing air temperature (i.e., thermal sensitivity). Previous efforts to forecast climate effects on brook trout (Salvelinus fontinalis) habitat have generally assumed uniform air-water temperature relationships over large areas that cannot account for groundwater inputs and other processes that operate at finer spatial scales. We developed regression models that accounted for groundwater influences on thermal sensitivity from measured air-water temperature relationships within forested watersheds in eastern North America (Shenandoah National Park, Virginia, USA, 78 sites in nine watersheds). We used these reach-scale models to forecast climate change effects on stream temperature and brook trout thermal habitat, and compared our results to previous forecasts based upon large-scale models. Observed stream temperatures were generally less sensitive to air temperature than previously assumed, and we attribute this to the moderating effect of shallow groundwater inputs. Predicted groundwater temperatures from air-water regression models corresponded well to observed groundwater temperatures elsewhere in the study area. Predictions of brook trout future habitat loss derived from our fine-grained models. were far less pessimistic than those from prior models developed at coarser spatial resolutions. However, our models also revealed spatial variation in thermal sensitivity within and among catchments resulting in a patchy distribution of thermally suitable habitat. Habitat fragmentation due to thermal barriers therefore may have an increasingly important role for trout population viability in headwater streams. Our results demonstrate that simple adjustments to air-water temperature regression models can provide a powerful and cost-effective approach for predicting future stream temperatures while accounting for effects of groundwater.

摘要

预测气候变化对水生动物及其栖息地的影响需要了解水温如何对空气温度变化(即热敏感性)作出响应。先前预测气候变化对溪红点鲑(Salvelinus fontinalis)栖息地影响的努力通常假设在大面积范围内空气-水温度关系是均匀的,而无法解释地下水输入和其他在更精细空间尺度上运行的过程。我们开发了回归模型,这些模型考虑了在北美东部(美国弗吉尼亚州的谢南多厄国家公园,9 个流域的 78 个地点)的森林流域内测量的空气-水温度关系对热敏感性的地下水影响。我们使用这些河段尺度模型来预测气候变化对溪流温度和溪红点鲑热栖息地的影响,并将我们的结果与基于大尺度模型的先前预测进行了比较。观测到的溪流温度通常比以前假设的对空气温度的敏感性要低,我们将这归因于浅层地下水输入的调节作用。从空气-水回归模型预测的地下水温度与研究区域其他地方观测到的地下水温度非常吻合。从我们的细粒度模型得出的未来溪红点鲑栖息地丧失的预测,远不如以前在较粗空间分辨率下开发的模型的预测悲观。然而,我们的模型还揭示了流域内和流域之间热敏感性的空间变化,导致了热适宜栖息地的斑块状分布。因此,由于热屏障导致的栖息地破碎化可能对溪流上游的鳟鱼种群生存力越来越重要。我们的研究结果表明,对空气-水温度回归模型进行简单调整,可以提供一种强大而具有成本效益的方法来预测未来的溪流温度,同时考虑地下水的影响。

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