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Climate change impact on the hydrology of Spencer Creek watershed in Southern Ontario, Canada

机译:气候变化对加拿大安大略省南部Spencer Creek流域水文学的影响

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This study is for the assessment of climate change impact on the future hydrology of Spencer Creek watershed located in Southern Ontario, Canada under the A2 scenario of the Special Report on Emissions Scenarios (SRES). The study is particularly concerned with changes in the climate variables and the seasonal and interannual flow regimes of the study area. The analysis also addresses the annual exceedance probability of extreme precipitation, temperature and flow events. Potential hydrologic effects of climate change were assessed for the Spencer Creek by imposing changes in precipitation and temperature derived from the North American Regional Climate Change Assessment Program (NARCCAP) climate simulations between 2040 and 2069. The climate models results were used as input to three hydrological models to produce projections of Spencer Creek watershed discharges. The results were compared to the observed discharges between 1989 and 2008. Notwithstanding the variability between the different regional climate model and hydrological model projections that envelop the future climate scenarios and the hydrological modeling uncertainties, all future simulations show an increase in the average interannual discharge, but also a noteworthy change in the seasonal distribution of the discharges. While the former is mainly attributed to the average annual precipitation, which tends to increase, the change in seasonal distribution of discharges is in line with the temperature increase of the winter and spring seasons that results in earlier snowmelt. Important changes were found in the annual exceedance probability (recurrence interval) of the extreme precipitation, temperature and runoff events.
机译:这项研究旨在评估在排放情景特别报告(SRES)的A2情景下,气候变化对位于加拿大安大略省南部的Spencer Creek流域未来水文学的影响。该研究特别关注气候变量的变化以及研究区域的季节和年际流量状况。该分析还解决了极端降水,温度和流量事件的年度超标概率。通过施加2040年至2069年间北美区域气候变化评估计划(NARCCAP)气候模拟得出的降水和温度变化,对斯宾塞河的气候变化潜在的水文影响进行了评估。气候模型结果被用作三个水文的输入模型以生成Spencer Creek流域流量的投影。将结果与1989年至2008年之间观测到的排放量进行了比较。尽管不同的区域气候模型与水文模型预测之间存在差异,但它们涵盖了未来的气候情景和水文模型的不确定性,所有未来的模拟都显示年平均排放量有所增加,而且排放量的季节性分布也有显着变化。前者主要归因于年平均降水量,而后者倾向于增加,但流量的季节性分布变化与冬季和春季的温度升高相一致,从而导致融雪较早。在极端降水,温度和径流事件的年度超标概率(重复间隔)中发现了重要的变化。

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