Increasing threat of coastal groundwater hazards from sea-level rise in California

被引:85
|
作者
Befus, K. M. [1 ,2 ]
Barnard, P. L. [3 ]
Hoover, D. J. [3 ]
Hart, J. A. Finzi [3 ]
Voss, C., I [4 ]
机构
[1] Univ Wyoming, Dept Civil & Architectural Engn, Laramie, WY 82071 USA
[2] Univ Arkansas, Dept Geosci, Fayetteville, AR 72701 USA
[3] US Geol Survey, Pacific Coastal & Marine Sci Ctr, Santa Cruz, CA USA
[4] US Geol Survey, Water Mission Area, 345 Middlefield Rd, Menlo Pk, CA 94025 USA
关键词
SEAWATER INTRUSION; WATER FLOW; IMPACT; DYNAMICS; VULNERABILITY; PERMEABILITY; SALINITY; AQUIFERS; GLHYMPS; TABLE;
D O I
10.1038/s41558-020-0874-1
中图分类号
X [环境科学、安全科学];
学科分类号
08 ; 0830 ;
摘要
Projected sea-level rise will raise coastal water tables, resulting in groundwater hazards that threaten shallow infrastructure and coastal ecosystem resilience. Here we model a range of sea-level rise scenarios to assess the responses of water tables across the diverse topography and climates of the California coast. With 1 m of sea-level rise, areas flooded from below are predicted to expand similar to 50-130 m inland, and low-lying coastal communities such as those around San Francisco Bay are most at risk. Coastal topography is a controlling factor; long-term rising water tables will intercept low-elevation drainage features, allowing for groundwater discharge that damps the extent of shoaling in similar to 70% (68.9-82.2%) of California's coastal water tables. Ignoring these topography-limited responses increases flooded-area forecasts by similar to 20% and substantially underestimates saltwater intrusion. All scenarios estimate that areas with shallow coastal water tables will shrink as they are inundated by overland flooding or are topographically limited from rising inland.
引用
收藏
页码:946 / +
页数:16
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