Alignment between water inputs and vegetation green-up reduces next year's runoff efficiency

IF 3.2 3区 地球科学 Q1 Environmental Science Hydrological Processes Pub Date : 2024-06-27 DOI:10.1002/hyp.15211
Sarah K. Newcomb, Robert W. Van Kirk, Sarah E. Godsey, Maggi Kraft
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Abstract

In the western United States, water supplies largely originate as snowmelt from forested land. Forests impact the water balance of these headwater streams, yet most predictive runoff models do not explicitly account for changing snow-vegetation dynamics. Here, we present a case study showing how warmer temperatures and changing forests in the Henrys Fork of the Snake River, a seasonally snow-covered headwater basin in the Greater Yellowstone Ecosystem, have altered the relationship between April 1st snow water equivalent (SWE) and summer streamflow. Since the onset and recovery of severe drought in the early 2000s, predictive models based on pre-drought relationships over-predict summer runoff in all three headwater tributaries of the Henrys Fork, despite minimal changes in precipitation or snow accumulation. Compared with the pre-drought period, late springs and summers (May–September) are warmer and vegetation is greener with denser forests due to recovery from multiple historical disturbances. Shifts in the alignment of snowmelt and energy availability due to warmer temperatures may reduce runoff efficiency by changing the amount of precipitation that goes to evapotranspiration versus runoff and recharge. To quantify the alignment between snowmelt and energy on a timeframe needed for predictive models, we propose a new metric, the Vegetation-Water Alignment Index (VWA), to characterize the synchrony of vegetation greenness and snowmelt and rain inputs. New predictive models show that in addition to April 1st SWE, the previous year's VWA and summer reference evapotranspiration are the most significant predictors of runoff in each watershed and provide more predictive power than traditionally used metrics. These results suggest that the timing of snowmelt relative to the start of the growing season affects not only annual partitioning of streamflow, but can also determine the groundwater storage state that dictates runoff efficiency the following spring.

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水输入与植被绿化之间的协调可降低下一年的径流效率
在美国西部,水源主要来自林地的融雪。森林会影响这些上游溪流的水量平衡,但大多数预测性径流模型并没有明确考虑到积雪-植被动态的变化。在这里,我们通过一个案例研究,展示了气温升高和森林变化如何改变了大黄石生态系统中季节性积雪覆盖的蛇河亨利岔流(Henrys Fork of the Snake River)上游流域 4 月 1 日的雪水当量(SWE)与夏季溪流之间的关系。自 2000 年代初严重干旱发生和恢复以来,尽管降水量或积雪量变化极小,但基于干旱前关系的预测模型对亨利斯岔道所有三条上游支流的夏季径流预测过高。与干旱前相比,春末和夏季(5 月至 9 月)更温暖,植被更绿,森林更茂密,这是从历史上的多次干扰中恢复过来的。由于气温升高,融雪与能量供应之间的关系发生了变化,这可能会改变用于蒸散的降水量与用于径流和补给的降水量,从而降低径流效率。为了在预测模型所需的时间范围内量化融雪和能量之间的一致性,我们提出了一个新的指标--植被-水一致性指数(VWA),以描述植被绿度与融雪和降雨输入的同步性。新的预测模型显示,除了 4 月 1 日的 SWE 外,上一年的 VWA 和夏季参考蒸散量是各流域径流最重要的预测指标,比传统使用的指标更具预测能力。这些结果表明,相对于生长季节开始的融雪时间不仅会影响每年的溪流分区,还会决定地下水的储存状态,从而决定第二年春季的径流效率。
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来源期刊
Hydrological Processes
Hydrological Processes 环境科学-水资源
CiteScore
6.00
自引率
12.50%
发文量
313
审稿时长
2-4 weeks
期刊介绍: Hydrological Processes is an international journal that publishes original scientific papers advancing understanding of the mechanisms underlying the movement and storage of water in the environment, and the interaction of water with geological, biogeochemical, atmospheric and ecological systems. Not all papers related to water resources are appropriate for submission to this journal; rather we seek papers that clearly articulate the role(s) of hydrological processes.
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