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Coupling instrumental and geological records of sea-level change: Evidence from southern New England of an increase in the rate of sea-level rise in the late 19th century
Geology and Geophysics Department, Woods Hole Oceanographic Institution, Woods Hole, Massachusetts, USA
Department of Geological Sciences, Brown University, Providence, Rhode Island, USA
Department of Environmental Sciences, University of Virginia, Charlottesville, Virginia, USA
Department of Geological Sciences, Brown University, Providence, Rhode Island, USA
Department of Geological Sciences, Brown University, Providence, Rhode Island, USA
We construct a high-resolution relative sea-level record for the past 700 years by dating basal salt-marsh peat samples above a glacial erratic in an eastern Connecticut salt marsh, to test whether or not the apparent recent acceleration in the rate of sea-level rise (SLR) is coeval with climate warming. The data reveal an average SLR rate of 1.0 ± 0.2 mm/year from about 1300 to 1850 A.D. Coupling of the regional tide-gauge data (1856 to present) with this marsh-based record indicates that the nearly three-fold increase in the regional rate of SLR to modern levels likely occurred in the later half of the 19th century. Thus the timing of the observed SLR rate increase is coincident with the onset of climate warming, indicating a possible link between historic SLR increases and recent temperature increases.
Received 27 October 2003; accepted 20 January 2004; published 11 March 2004.
Citation: (2004), Coupling instrumental and geological records of sea-level change: Evidence from southern New England of an increase in the rate of sea-level rise in the late 19th century, Geophys. Res. Lett., 31, L05203, doi:10.1029/2003GL018933.
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