Matches in SemOpenAlex for { <https://semopenalex.org/work/W2891499209> ?p ?o ?g. }
- W2891499209 endingPage "2291" @default.
- W2891499209 startingPage "2279" @default.
- W2891499209 abstract "Abstract A coupled ice sheet‐Earth‐sea level model is used to estimate the modern elevations of shoreline features that were formed at high sea level stands during the warm mid Pliocene ~3 million years ago. Knowledge of global mean sea level during this period is important as an indicator of possible future ice sheet retreat and sea level rise. However, local shoreline elevations can deviate from the eustatic mean by various geologic processes over the last 3 million years, including glacial isostatic adjustment of the solid Earth and gravitational field due to both Pliocene ice‐cover changes and more recent glacial cycles. Our coupled model includes glacial isostatic adjustment processes and simulates Antarctic ice sheet, global sea level, and solid Earth variations in the warmest mid‐Pliocene and over the last 40,000 years. Global maps of estimated modern elevations of Pliocene shoreline markers are produced for a standard radial profile of Earth viscosity and lithospheric thickness. Results are compared to an earlier study with an uncoupled Earth‐sea level model and a different methodology (Raymo et al., Nature Geoscience, 2011, https://doi.org:/10.1038/ngeo1118 ). As in that study, Pliocene shoreline elevations diverge significantly from the eustatic value in widespread regions, especially in the vicinity of present and former ice sheets. In some other regions, elevations are close to eustatic. The results emphasize that care should be taken in interpreting elevations of paleo‐shoreline markers." @default.
- W2891499209 created "2018-09-27" @default.
- W2891499209 creator A5001243017 @default.
- W2891499209 creator A5003897779 @default.
- W2891499209 creator A5075221789 @default.
- W2891499209 creator A5080211058 @default.
- W2891499209 date "2018-09-01" @default.
- W2891499209 modified "2023-10-16" @default.
- W2891499209 title "Estimating Modern Elevations of Pliocene Shorelines Using a Coupled Ice Sheet‐Earth‐Sea Level Model" @default.
- W2891499209 cites W1514237529 @default.
- W2891499209 cites W1630818818 @default.
- W2891499209 cites W1675281091 @default.
- W2891499209 cites W1964286915 @default.
- W2891499209 cites W1965075827 @default.
- W2891499209 cites W1968247562 @default.
- W2891499209 cites W1971799755 @default.
- W2891499209 cites W1981304827 @default.
- W2891499209 cites W1988975008 @default.
- W2891499209 cites W1989177281 @default.
- W2891499209 cites W1996658865 @default.
- W2891499209 cites W2002937458 @default.
- W2891499209 cites W2005800145 @default.
- W2891499209 cites W2016667544 @default.
- W2891499209 cites W2020504130 @default.
- W2891499209 cites W2025833891 @default.
- W2891499209 cites W2025997795 @default.
- W2891499209 cites W2030685468 @default.
- W2891499209 cites W2043250480 @default.
- W2891499209 cites W2062221814 @default.
- W2891499209 cites W2069620066 @default.
- W2891499209 cites W2072935186 @default.
- W2891499209 cites W2075165785 @default.
- W2891499209 cites W2083732652 @default.
- W2891499209 cites W2087405923 @default.
- W2891499209 cites W2094033454 @default.
- W2891499209 cites W2097914838 @default.
- W2891499209 cites W2101720402 @default.
- W2891499209 cites W2101875061 @default.
- W2891499209 cites W2102213705 @default.
- W2891499209 cites W2112363056 @default.
- W2891499209 cites W2122292225 @default.
- W2891499209 cites W2127610390 @default.
- W2891499209 cites W2133855861 @default.
- W2891499209 cites W2137966020 @default.
- W2891499209 cites W2140477756 @default.
- W2891499209 cites W2142446883 @default.
- W2891499209 cites W2147966841 @default.
- W2891499209 cites W2149432953 @default.
- W2891499209 cites W2149606039 @default.
- W2891499209 cites W2153259684 @default.
- W2891499209 cites W2166411116 @default.
- W2891499209 cites W2194439098 @default.
- W2891499209 cites W2269759485 @default.
- W2891499209 cites W2291649384 @default.
- W2891499209 cites W2306905182 @default.
- W2891499209 cites W2320249130 @default.
- W2891499209 cites W2506367938 @default.
- W2891499209 cites W2568256832 @default.
- W2891499209 cites W2617851267 @default.
- W2891499209 cites W2741413404 @default.
- W2891499209 cites W2762170052 @default.
- W2891499209 cites W2765158146 @default.
- W2891499209 cites W2788534139 @default.
- W2891499209 cites W4306293736 @default.
- W2891499209 cites W85906244 @default.
- W2891499209 doi "https://doi.org/10.1029/2018jf004745" @default.
- W2891499209 hasPublicationYear "2018" @default.
- W2891499209 type Work @default.
- W2891499209 sameAs 2891499209 @default.
- W2891499209 citedByCount "5" @default.
- W2891499209 countsByYear W28914992092019 @default.
- W2891499209 countsByYear W28914992092020 @default.
- W2891499209 countsByYear W28914992092021 @default.
- W2891499209 countsByYear W28914992092022 @default.
- W2891499209 crossrefType "journal-article" @default.
- W2891499209 hasAuthorship W2891499209A5001243017 @default.
- W2891499209 hasAuthorship W2891499209A5003897779 @default.
- W2891499209 hasAuthorship W2891499209A5075221789 @default.
- W2891499209 hasAuthorship W2891499209A5080211058 @default.
- W2891499209 hasBestOaLocation W28914992091 @default.
- W2891499209 hasConcept C100970517 @default.
- W2891499209 hasConcept C111368507 @default.
- W2891499209 hasConcept C123750103 @default.
- W2891499209 hasConcept C127313418 @default.
- W2891499209 hasConcept C134543767 @default.
- W2891499209 hasConcept C136894858 @default.
- W2891499209 hasConcept C140711978 @default.
- W2891499209 hasConcept C151730666 @default.
- W2891499209 hasConcept C152382732 @default.
- W2891499209 hasConcept C15739521 @default.
- W2891499209 hasConcept C16942324 @default.
- W2891499209 hasConcept C180705331 @default.
- W2891499209 hasConcept C197435368 @default.
- W2891499209 hasConcept C205649164 @default.
- W2891499209 hasConcept C2780223605 @default.
- W2891499209 hasConcept C49204034 @default.
- W2891499209 hasConcept C74501621 @default.
- W2891499209 hasConcept C77928131 @default.