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卫星揭示全球河流延伸变化的热点。

Satellites reveal hotspots of global river extent change.

机构信息

Key Laboratory of Watershed Geographic Sciences, Nanjing Institute of Geography and Limnology, Chinese Academy of Sciences, Nanjing, 210008, China.

School of Biological Sciences and Institute for Climate and Carbon Neurality, The University of Hong Kong, Pokfulam Road, Hong Kong, China.

出版信息

Nat Commun. 2023 Mar 22;14(1):1587. doi: 10.1038/s41467-023-37061-3.

Abstract

Rivers are among the most diverse, dynamic, and productive ecosystems on Earth. River flow regimes are constantly changing, but characterizing and understanding such changes have been challenging from a long-term and global perspective. By analyzing water extent variations observed from four-decade Landsat imagery, we here provide a global attribution of the recent changes in river regime to morphological dynamics (e.g., channel shifting and anabranching), expansion induced by new dams, and hydrological signals of widening and narrowing. Morphological dynamics prevailed in ~20% of the global river area. Booming reservoir constructions, mostly skewed in Asia and South America, contributed to ~32% of the river widening. The remaining hydrological signals were characterized by contrasting hotspots, including prominent river widening in alpine and pan-Arctic regions and narrowing in the arid/semi-arid continental interiors, driven by varying trends in climate forcing, cryospheric response to warming, and human water management. Our findings suggest that the recent river extent dynamics diverge based on hydroclimate and socio-economic conditions, and besides reflecting ongoing morphodynamical processes, river extent changes show close connections with external forcings, including climate change and anthropogenic interference.

摘要

河流是地球上最多样化、最具活力和生产力的生态系统之一。河川水流模式一直在不断变化,但从长期和全球角度来描述和理解这些变化一直具有挑战性。通过分析过去四十年 Landsat 图像观测到的水域范围变化,我们在此对近期河川水流模式的变化进行了全球归因分析,这些变化归因于形态动力学(例如河道迁移和叉流)、新水坝扩张以及河道展宽和收窄的水文信号。形态动力学在全球约 20%的河流流域中占主导地位。亚洲和南美洲的水库建设蓬勃发展,导致约 32%的河流展宽。其余的水文信号则以鲜明的热点为特征,包括高山和泛北极地区的河流展宽以及干旱/半干旱大陆内部的河流收窄,这是由气候驱动因素、变暖对冰冻圈的响应以及人为水资源管理的不同趋势所驱动的。我们的研究结果表明,近期的河流范围动态变化取决于水文气候和社会经济条件,并且除了反映正在进行的形态动力学过程外,河流范围的变化还与外部强迫因素密切相关,包括气候变化和人为干扰。

https://cdn.ncbi.nlm.nih.gov/pmc/blobs/34be/10033638/c2c535f4e263/41467_2023_37061_Fig1_HTML.jpg

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