人类活动导致的全球旱地地表水储存与降水的解耦

Gang Zhao, Huilin Gao, Yao Li, Qiuhong Tang, R. Iestyn Woolway, Julian Merder, Lorenzo Rosa, Anna M. Michalak
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引用次数: 0

摘要

全球旱地地表水的可用性对人类社会和生态系统都至关重要。然而,地表水储存变化的长期驱动因素,特别是那些与人为活动有关的因素,仍然不清楚。本文利用多任务遥感数据,构建了1985 - 2020年全球105,400个旱地湖泊和水库的月度储水量变化时间序列。地表水储存量每年增加2.20立方千米,主要是由于新水库的建设。相反,对于湖泊和旧水库(建于1983年以前),从全球总量来看,储水量的趋势不大,但在全球91%的单个旱地盆地中,它们主导着地表水的储水量趋势。进一步的分析表明,这些水体的长期储存变化主要与人为因素有关,包括人为引起的变暖和水资源管理实践,而不是像以前认为的那样与降水变化有关。这些发现揭示了全球旱地地表水储存与降水的脱钩,引起了对社会和生态系统可持续性的关注。本文对1985-2020年全球旱地流域地表水储量变化进行了量化和归因,表明长期变化主要与人为因素有关,而与降水无关。
本文章由计算机程序翻译,如有差异,请以英文原文为准。

Decoupling of surface water storage from precipitation in global drylands due to anthropogenic activity

Decoupling of surface water storage from precipitation in global drylands due to anthropogenic activity
The availability of surface water in global drylands is essential for both human society and ecosystems. However, the long-term drivers of change in surface water storage, particularly those related to anthropogenic activities, remain unclear. Here we use multi-mission remote sensing data to construct monthly time series of water storage changes from 1985 to 2020 for 105,400 lakes and reservoirs in global drylands. An increase of 2.20 km3 per year in surface water storage is found primarily due to the construction of new reservoirs. For lakes and old reservoirs (constructed before 1983), conversely, the trend in storage is minor when aggregated globally, but they dominate surface water storage trends in 91% of individual global dryland basins. Further analysis reveals that long-term storage changes in these water bodies are primarily linked to anthropogenic factors—including human-induced warming and water-management practices—rather than to precipitation changes, as previously thought. These findings reveal a decoupling of surface water storage from precipitation in global drylands, raising concerns about societal and ecosystem sustainability. This study quantifies and attributes the changes of surface water storage in global dryland basins over 1985–2020, indicating that long-term changes are mainly linked to anthropogenic factors rather than precipitation.
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