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Consequences of declining snow accumulation for water balance of mid-latitude dry regions

机译:积雪减少对中纬度干旱地区水量平衡的影响

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Widespread documentation of positive winter temperature anomalies, declining snowpack and earlier snow melt in the Northern Hemisphere have raised concerns about the consequences for regional water resources as well as wildfire. A topic that has not been addressed with respect to declining snowpack is effects on ecosystem water balance. Changes in water balance dynamics will be particularly pronounced at low elevations of mid-latitude dry regions because these areas will be the first to be affected by declining snow as a result of rising temperatures. As a model system, we used simulation experiments to investigate big sagebrush ecosystems that dominate a large fraction of the semiarid western United States. Our results suggest that effects on future ecosystem water balance will increase along a climatic gradient from dry, warm and snow-poor to wet, cold and snow-rich. Beyond a threshold within this climatic gradient, predicted consequences for vegetation switched from no change to increasing transpiration. Responses were sensitive to uncertainties in climatic prediction; particularly, a shift of precipitation to the colder season could reduce impacts of a warmer and snow-poorer future, depending on the degree to which ecosystem phenology tracks precipitation changes. Our results suggest that big sagebrush and other similar semiarid ecosystems could decrease in viability or disappear in dry to medium areas and likely increase only in the snow-richest areas, i.e. higher elevations and higher latitudes. Unlike cold locations at high elevations or in the arctic, ecosystems at low elevations respond in a different and complex way to future conditions because of opposing effects of increasing water-limitation and a longer snow-free season. Outcomes of such nonlinear interactions for future ecosystems will likely include changes in plant composition and productivity, dynamics of water balance, and availability of water resources.
机译:关于北半球冬季正温度异常,积雪减少和较早融雪的广泛文献引起了人们对区域水资源和野火后果的担忧。关于降雪量尚未解决的一个话题是对生态系统水平衡的影响。在中纬度干旱地区的低海拔地区,水平衡动态的变化尤为明显,因为这些地区将是第一个受气温上升而降雪影响的地区。作为模型系统,我们使用模拟实验研究了占主导地位的美国半干旱西部大部分的大型鼠尾草生态系统。我们的结果表明,对未来生态系统水平衡的影响将沿着气候梯度从干燥,温暖和积雪少到潮湿,寒冷和积雪多的气候梯度增加。在此气候梯度范围内,超出阈值的植被预计后果将从无变化转为蒸腾。反应对气候预测的不确定性敏感;尤其是,将降水转移到较冷的季节可能会减少更暖和更雪的未来的影响,具体取决于生态系统物候对降水变化的跟踪程度。我们的研究结果表明,大型鼠尾草和其他类似的半干旱生态系统可能会在干旱至中度地区生存能力下降或消失,并且可能仅在雪最丰富的地区(即更高的海拔和更高的纬度)才会增加。与高海拔地区或北极的寒冷地区不同,低海拔地区的生态系统以不同和复杂的方式对未来状况做出响应,这是由于水限制增加和无雪季节更长的不利影响。这种对未来生态系统的非线性相互作用的结果可能包括植物组成和生产力的变化,水平衡的动态变化以及水资源的可获得性。

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