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- W4317367946 abstract "Abstract Sea level changed with CO2 over the past 500 million years in response to plate tectonic forcing (abundant mid-ocean ridges provide CO2, and raise sea level). Sea level is thus a barometer of Earth’s climate states, falling as ice sheets grow. Following Milankovitch Cycles of insolation, it fluctuated with ice volume and CO2 throughout the Pleistocene ice age. During the Anthropocene, deltas (human breadbaskets) are being flooded (1) by meltwater contributions, and (2) due to subsidence caused by the cutting off of their supply of silt by dams upstream. The rate of global sea level rise has accelerated to 4 mm/yr (c. 3/16 of an inch/yr). Rises of up to c.1.8 m (5.9 ft) are expected by 2100 as the world warms, possibly reaching 10–14 m (33–46 ft) in the 300-year time frame, as occurred in Pliocene times. Where ice is melting, sea level will fall as the land rises, relieved of its icy burden." @default.
- W4317367946 created "2023-01-19" @default.
- W4317367946 creator A5001313270 @default.
- W4317367946 date "2023-02-20" @default.
- W4317367946 modified "2023-09-23" @default.
- W4317367946 title "Rising Seas" @default.
- W4317367946 doi "https://doi.org/10.1093/oso/9780197627983.003.0008" @default.
- W4317367946 hasPublicationYear "2023" @default.
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