Coastal subsidence and relative sea level rise
Subsurface fluid-pressure declines caused by pumping of groundwater or hydrocarbons can lead to aquifer-system compaction and consequent land subsidence. This subsidence can be rapid, as much as 30 cm per year in some instances, and large, totaling more than 13 m in extreme examples. Thus anthropoge...
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| Veröffentlicht in: | Environmental research letters 2014-09, Vol.9 (9), p.91002 |
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| creator | Ingebritsen, S E Galloway, D L |
| description | Subsurface fluid-pressure declines caused by pumping of groundwater or hydrocarbons can lead to aquifer-system compaction and consequent land subsidence. This subsidence can be rapid, as much as 30 cm per year in some instances, and large, totaling more than 13 m in extreme examples. Thus anthropogenic subsidence may be the dominant contributor to relative sea-level rise in coastal environments where subsurface fluids are heavily exploited. Maximum observed rates of human-induced subsidence greatly exceed the rates of natural subsidence of unconsolidated sediments (∼0.1-1 cm yr−1) and the estimated rates of ongoing global sea-level rise (∼0.3 cm yr−1). |
| doi_str_mv | 10.1088/1748-9326/9/9/091002 |
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| subjects | Anthropogenic factors Aquifers coastal Coastal environments Groundwater Human influences Land subsidence Sea level rise Sediments Subsidence |
| title | Coastal subsidence and relative sea level rise |
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