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最近在北美西部的积雪水储量下降
Katherine E Hale1,2,3, Keith S Jennings4, Keith N Musselman1,2
1Department of Geography, University of Colorado at Boulder, Boulder, CO USA.
概括
山上的雪地是重要的水资源. 一个新的雪储量指数 (SSI) 显示北美西部的雪地储量正在下降,由于早些时候的融雪和降水减少,这影响了水的可用性.
科学领域:
- 水文学的水文学
- 气候学 气候学 气候学
- 环境科学 环境科学
背景情况:
- 山上积雪地充当了重要的自然水库,储存降水,在夏季更干燥的月份释放.
- 了解雪水储存对于管理水资源至关重要,尤其是在季节性需求较高的地区.
研究的目的:
- 引入一种新型指标,即雪积分指数 (SSI),用于量化雪积水储存动态.
- 分析北美西部雪水储存的长期趋势.
主要方法:
- 开发了雪积分指数 (SSI),以测量降水和地表水输入 (融雪和降雨) 之间的时间相差.
- 分析了北美西部山区的1950-2013年年度SSI趋势.
主要成果:
- 在1950年至2013年期间,北美西部山区的25%以上的地区,每年的SSI下降了.
- 观察到的SSI下降归因于早春的融雪和降雨,以及冬季降水量减少.
结论:
- 降低的SSI表明积雪积延迟水供应的能力下降,这给水资源管理带来了挑战.
- 这些发现凸显了山区对气候变化的水文敏感性,对生态系统和供水有重大影响.
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