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• W1568157070 abstract "[1] Along the eastern seaboard of the U.S. from Florida to Maine, sea level rise (SLR) shows notable patterns and significant deviation from the global mean, which have been attributed to land subsidence. Consistent with several recent studies, we analyze various observation and modeling data, and find that ocean dynamics is also an important factor in explaining these coastal SLR patterns. Despite a southward shift since the 1990s, an overall northward shift of the Gulf Stream during the twentieth century contributed to the faster SLR in the Mid-Atlantic region (North Carolina to New Jersey). In response to the 21st century climatic forcing, the rise (fall) of the dynamic sea level north (south) of Cape Hatteras is mainly induced by the significant decline of ocean density contrast across the Gulf Stream. This baroclinic process is the likely cause of the recent switch of the coastal SLR to a pattern with faster (slower) rates north (south) of Cape Hatteras." @default.
• W1568157070 created "2016-06-24" @default.
• W1568157070 creator A5005091220 @default.
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• W1568157070 date "2013-10-25" @default.
• W1568157070 modified "2023-10-01" @default.
• W1568157070 title "Oceanic control of sea level rise patterns along the East Coast of the United States" @default.
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• W1568157070 doi "https://doi.org/10.1002/2013gl057992" @default.
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