Department of Land, Air, and Water Resources, University of California, Davis, CA, USA.
Sci Total Environ. 2013 Apr 15;450-451:72-82. doi: 10.1016/j.scitotenv.2013.02.004. Epub 2013 Mar 1.
The assessment of hydrologic responses to climate change is required in watershed management and planning to protect water resources and environmental quality. This study is designed to evaluate and enhance watershed modeling approach in characterizing climate change impacts on water supply and ecosystem stressors. Soil and Water Assessment Tool (SWAT) was selected as a base model, and improved for the CO2 dependence of potential evapotranspiration and stream temperature prediction. The updated model was applied to quantify the impacts of projected 21st century climate change in the northern Coastal Ranges and western Sierra Nevada, which are important water source areas and aquatic habitats of California. Evapotranspiration response to CO2 concentration varied with vegetation type. For the forest-dominated watersheds in this study, only moderate (1-3%) reductions on evapotranspiration were predicted by solely elevating CO2 concentration under emission scenarios A2 and B1. Modeling results suggested increases in annual average stream temperature proportional to the projected increases in air temperature. Although no temporal trend was confirmed for annual precipitation in California, increases of precipitation and streamflow during winter months and decreases in summers were predicted. Decreased streamflow during summertime, together with the higher projected air temperature in summer than in winter, would increase stream temperature during those months and result in unfavorable conditions for cold-water species. Compared to the present-day conditions, 30-60 more days per year were predicted with average stream temperature >20°C during 2090s. Overall, the hydrologic cycle and water quality of headwater drainage basins of California, especially their seasonality, are very sensitive to projected climate change.
气候变化对水文响应的评估是流域管理和规划的要求,以保护水资源和环境质量。本研究旨在评估和增强流域模型方法,以描述气候变化对供水和生态胁迫因素的影响。选择土壤和水评估工具(SWAT)作为基础模型,并对其进行改进,以考虑潜在蒸散量对 CO2 的依赖性和预测溪流温度。更新后的模型用于量化加利福尼亚北部沿海山脉和西部内华达山脉 21 世纪气候变化预测的影响,这些地区是加利福尼亚重要的水源地和水生栖息地。CO2 浓度对蒸散的响应因植被类型而异。对于本研究中以森林为主的流域,仅在排放情景 A2 和 B1 下,仅通过升高 CO2 浓度,预计蒸散量将减少 1-3%。模型结果表明,年平均溪流温度将随预计的空气温度升高而增加。尽管加利福尼亚的年降水量没有时间趋势,但预计冬季降水量和径流量增加,夏季减少。夏季径流量减少,加上夏季空气温度高于冬季,将导致这些月份的溪流温度升高,对冷水物种不利。与现状相比,预计在 2090 年代,每年将有 30-60 天以上的时间平均溪流温度>20°C。总体而言,加利福尼亚上游流域的水文循环和水质,尤其是其季节性,对预测的气候变化非常敏感。