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人类对全球地表水存储变异性的改变。

Human alteration of global surface water storage variability.

机构信息

Department of Earth System Science, Stanford University, Stanford, CA, USA.

Department of Geography, University of Oregon, Eugene, OR, USA.

出版信息

Nature. 2021 Mar;591(7848):78-81. doi: 10.1038/s41586-021-03262-3. Epub 2021 Mar 3.

Abstract

Knowing the extent of human influence on the global hydrological cycle is essential for the sustainability of freshwater resources on Earth. However, a lack of water level observations for the world's ponds, lakes and reservoirs has limited the quantification of human-managed (reservoir) changes in surface water storage compared to its natural variability. The global storage variability in surface water bodies and the extent to which it is altered by humans therefore remain unknown. Here we show that 57 per cent of the Earth's seasonal surface water storage variability occurs in human-managed reservoirs. Using measurements from NASA's ICESat-2 satellite laser altimeter, which was launched in late 2018, we assemble an extensive global water level dataset that quantifies water level variability for 227,386 water bodies from October 2018 to July 2020. We find that seasonal variability in human-managed reservoirs averages 0.86 metres, whereas natural water bodies vary by only 0.22 metres. Natural variability in surface water storage is greatest in tropical basins, whereas human-managed variability is greatest in the Middle East, southern Africa and the western USA. Strong regional patterns are also found, with human influence driving 67 per cent of surface water storage variability south of 45 degrees north and nearly 100 per cent in certain arid and semi-arid regions. As economic development, population growth and climate change continue to pressure global water resources, our approach provides a useful baseline from which ICESat-2 and future satellite missions will be able to track human modifications to the global hydrologic cycle.

摘要

了解人类对全球水文循环的影响程度对于地球淡水资源的可持续性至关重要。然而,由于缺乏对世界池塘、湖泊和水库水位的观测,与自然变率相比,人类管理(水库)对地表水储存变化的量化受到限制。因此,地表水体的全球储存变率及其受人类影响的程度仍然未知。在这里,我们表明,地球季节性地表水储存变率的 57%发生在人类管理的水库中。利用美国宇航局(NASA)于 2018 年底发射的 ICESat-2 卫星激光高度计的测量结果,我们组装了一个广泛的全球水位数据集,该数据集量化了 2018 年 10 月至 2020 年 7 月期间 227386 个水体的水位变率。我们发现,人类管理的水库的季节性变率平均为 0.86 米,而自然水体的变率仅为 0.22 米。人类管理的水库的地表水储存季节性变率在热带流域最大,而在中东、南部非洲和美国西部最大。还发现了强烈的区域模式,在北纬 45 度以南,人类影响导致 67%的地表水储存变率,在某些干旱和半干旱地区,这一比例接近 100%。随着经济发展、人口增长和气候变化继续给全球水资源带来压力,我们的方法提供了一个有用的基线,ICESat-2 和未来的卫星任务将能够跟踪人类对全球水文循环的修改。

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