Spatial variability of late Holocene and 20th century sea-level rise along the Atlantic coast of the United States
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Material Information

Title:
Spatial variability of late Holocene and 20th century sea-level rise along the Atlantic coast of the United States
Series Title:
Geology Volume 37
Creator:
Engelhart, Simon E.
Horton, Benjamin P.
Douglas, Bruce C.
Peltier, W. Richard
Tornqvist, Torbjorn E.
Publisher:
Geological Society of America
Publication Date:
Language:
English

Subjects

Subjects / Keywords:
Climate Change ( lcsh )
Sea Level Rise ( lcsh )
Atlantic Coast (U.S.) ( lcsh )

Notes

Abstract:
Accurate estimates of global sea-level rise in the pre-satellite era provide a context for 21st century sea-level predictions, but the use of tide-gauge records is complicated by the contributions from changes in land level due to glacial isostatic adjustment (GIA). We have constructed a rigorous quality-controlled database of late Holocene sea-level indices from the U.S. Atlantic coast, exhibiting subsidence rates of <0.8 mm a–1 in Maine, increasing to rates of 1.7 mm a–1 in Delaware, and a return to rates <0.9 mm a–1 in the Carolinas. This pattern can be attributed to ongoing GIA due to the demise of the Laurentide Ice Sheet. Our data allow us to defi ne the geometry of the associated collapsing proglacial forebulge with a level of resolution unmatched by any other currently available method. The corresponding rates of relative sea-level rise serve as background rates on which future sea-level rise must be superimposed. We further employ the geological data to remove the GIA component from tide-gauge records to estimate a mean 20th century sea-level rise rate for the U.S. Atlantic coast of 1.8 ± 0.2 mm a–1, similar to the global average. However, we fi nd a distinct spatial trend in the rate of 20th century sea-level rise, increasing from Maine to South Carolina. This is the fi rst evidence of this phenomenon from observational data alone. We suggest this may be related to the melting of the Greenland ice sheet and/or ocean steric effects. ( English )

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Florida International University
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Sea Level Rise