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- W2056524864 abstract "Vertical ground motion (VGM) rates stand as crucial information, either for predicting the impact of the actual sea level rise along low-lying coasts or refining geodynamic problems. Because present day VGM rates have a magnitude smaller than 10 mm/yr, they remain challenging to quantify and often elusive. We focus on the quantification of global-scale VGM rates in order to identify global or regional trends. We computed VGM rates by combining tide gauges records and local satellite altimetry, which yield a new dataset of 634 VGM rates. We further compare this database to previous studies that use geodetic techniques and tide gauges records in order to evaluate the consistency of both our results and previous ones. The magnitudes differ by less than 5 mm/yr, and similar subsidence and uplift general tendencies appear. Even if the asset of our database stands in the greater number of sites, the combination of all studies, each with different pros and cons, yields a hybrid dataset that makes our attempt to extract VGM trends more robust than any other, independent study. Fennoscandia, the West coast of North America, and the eastern coast of Australia are uplifting, while the eastern coast of North America, the British Isles and Western Europe, the eastern Mediterranean Sea, Japan, and the western coast of Australia are subsiding. Glacial Isostatic Adjustment (GIA) is expected to provide a major contribution to the present-day signal. Aside from Fennoscandia, observed VGM often depart from the GIA model predictions of Peltier (2004). This either results from an underestimate of the model predictions or from the influence of other processes: indeed, the influence of the geodynamic setting appears in particular along the coasts of western North America or Japan, where the alternation of transform faults and subduction zones makes it possible to assign contrasted behaviours to the local geodynamic context. Local mechanisms like anthropogenic processes or sediment compaction, also contribute to VGM. This remains true for the critical cases of Venice, the Gulf of Mexico, the Ganges delta, and the Maldives, which are particularly exposed to the current sea level rise." @default.
- W2056524864 created "2016-06-24" @default.
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- W2056524864 date "2012-01-01" @default.
- W2056524864 modified "2023-09-30" @default.
- W2056524864 title "Present-day trends of vertical ground motion along the coast lines" @default.
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- W2056524864 cites W1964821319 @default.
- W2056524864 cites W1965335989 @default.
- W2056524864 cites W1969666225 @default.
- W2056524864 cites W1971898795 @default.
- W2056524864 cites W1975972068 @default.
- W2056524864 cites W1978619457 @default.
- W2056524864 cites W1981900098 @default.
- W2056524864 cites W1982576506 @default.
- W2056524864 cites W1987613981 @default.
- W2056524864 cites W1988142685 @default.
- W2056524864 cites W2003161610 @default.
- W2056524864 cites W2006057327 @default.
- W2056524864 cites W2008715786 @default.
- W2056524864 cites W2009721490 @default.
- W2056524864 cites W2010988106 @default.
- W2056524864 cites W2018252114 @default.
- W2056524864 cites W2018314772 @default.
- W2056524864 cites W2018455263 @default.
- W2056524864 cites W2022415851 @default.
- W2056524864 cites W2023815011 @default.
- W2056524864 cites W2024375163 @default.
- W2056524864 cites W2026261813 @default.
- W2056524864 cites W2031010640 @default.
- W2056524864 cites W2035109608 @default.
- W2056524864 cites W2037079369 @default.
- W2056524864 cites W2038438522 @default.
- W2056524864 cites W2041320880 @default.
- W2056524864 cites W2043549294 @default.
- W2056524864 cites W2046922644 @default.
- W2056524864 cites W2053952330 @default.
- W2056524864 cites W2054591717 @default.
- W2056524864 cites W2065752147 @default.
- W2056524864 cites W2066277575 @default.
- W2056524864 cites W2069509807 @default.
- W2056524864 cites W2071118545 @default.
- W2056524864 cites W2073104124 @default.
- W2056524864 cites W2076954069 @default.
- W2056524864 cites W2079390700 @default.
- W2056524864 cites W2079870425 @default.
- W2056524864 cites W2081593086 @default.
- W2056524864 cites W2083018627 @default.
- W2056524864 cites W2085527155 @default.
- W2056524864 cites W2091893951 @default.
- W2056524864 cites W2094666610 @default.
- W2056524864 cites W2095046199 @default.
- W2056524864 cites W2096225198 @default.
- W2056524864 cites W2098679437 @default.
- W2056524864 cites W2101658891 @default.
- W2056524864 cites W2105766631 @default.
- W2056524864 cites W2107946076 @default.
- W2056524864 cites W2108273792 @default.
- W2056524864 cites W2109062369 @default.
- W2056524864 cites W2111107436 @default.
- W2056524864 cites W2112236890 @default.
- W2056524864 cites W2112363056 @default.
- W2056524864 cites W2112568224 @default.
- W2056524864 cites W2117871563 @default.
- W2056524864 cites W2124804051 @default.
- W2056524864 cites W2129084002 @default.
- W2056524864 cites W2131455151 @default.
- W2056524864 cites W2131539855 @default.
- W2056524864 cites W2137503015 @default.
- W2056524864 cites W2142446883 @default.
- W2056524864 cites W2143332220 @default.
- W2056524864 cites W2146315266 @default.
- W2056524864 cites W2147988117 @default.
- W2056524864 cites W2156337708 @default.
- W2056524864 cites W2164222045 @default.
- W2056524864 cites W2177237934 @default.
- W2056524864 cites W2219954581 @default.
- W2056524864 cites W4242995814 @default.
- W2056524864 doi "https://doi.org/10.1016/j.earscirev.2011.10.004" @default.
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