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Updated: Jun 25, 2025

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在雪的世界里流动的季节性
Juntai Han1,2, Ziwei Liu1,2, Ross Woods3
1State Key Laboratory of Hydroscience and Engineering, Department of Hydraulic Engineering, Tsinghua University, Beijing, China.
Nature
|May 29, 2024
概括
气候变暖将降雨量从降雪转变为降雨,影响河流流动时间. 与简单的模型相反,降雪率的下降会导致溪流的前进或延迟,这取决于积雪.
科学领域:
- 水文学
- 气候学
- 环境科学
背景情况:
- 气候变暖正在将寒冷地区从降雪转变为降雨,改变雪地动态,影响生态系统服务.
- 现有的模型表明降雪率下降导致较早的融雪和流动, 但这种反应是不确定的.
研究的目的:
- 对北半球降雪率下降的河流流程的复杂反应进行调查.
- 挑战简单的"较少的雪等于较早的流动"启发式.
主要方法:
- 分析了从1950年至2020年北半球3049个受雪影响的流域的流量测量.
- 研究了降雪量与流量质量中心的时间关系.
主要成果:
- 降雪率的下降会导致河流流动的时间提前或延迟.
- 河流流动的响应时间由平均降雪率调节,有丰富的积雪流域显示较早的河流流动,较少的积雪流域显示延迟的河流流动.
- 随着降雪率的下降,河流流动的年间变化和季节性变化会增加.
结论:
- 降雪量与河流流动时间之间的关系比之前的假设要复杂.
- 这些发现表明季节性流动模式的细微演变是对降低积雪的反应.
- 修改了对雪占主导地位的地区气候变化的水文反应的理解.
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