湿地
分水岭
沉积物
河口
水文学(农业)
环境科学
沉积预算
地质学
海洋学
仰角(弹道)
泥沙输移
生态学
地貌学
几何学
岩土工程
数学
机器学习
计算机科学
生物
作者
Scott H. Ensign,Joanne N. Halls,Erin Peck
出处
期刊:Science
[American Association for the Advancement of Science]
日期:2023-12-07
卷期号:382 (6675): 1191-1195
被引量:9
标识
DOI:10.1126/science.adj0513
摘要
Watershed sediment can increase elevation of tidal wetlands struggling against rising seas, but where and how much watershed sediment helps is unknown. By combining contiguous US datasets on sediment loads and tidal wetland areas for 4972 rivers and their estuaries, we calculated that river sediment accretion will be insufficient to match sea level rise in 72% of cases because most watersheds are too small (median 21 square kilometers) to generate adequate sediment. Nearly half the tidal wetlands would require 10 times more river sediment to match sea level, a magnitude not generally achievable by dam removal in some regions. The realization that watershed sediment has little effect on most tidal wetland elevations shifts research priorities toward biological processes and coastal sediment dynamics that most influence elevation change.
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