T146 Recent Sea-Level Rise: Accelerating or Not?
Tuesday, 6 November 2012
8:00 AM - 12:00 PM
218AB
SEA-LEVEL CHANGE ALONG THE ATLANTIC COAST OF THE UNITED STATES
Paper number: T146-6
Program: Technical Sessions
Time: 9:25 AM – 9:40 AM
Authors
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Andrew C. KempTufts University, Medford, MA
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J. DonnellyWoods Hole Oceanographic Institution, Woods Hole, MA
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Andrea D. HawkesUniversity of North Carolina Wilmington, Wilmington, NC
Abstract
Before the models can provide appropriate data for coastal management and planning, they must be complemented with regional estimates of sea-level rise. The proxy sea-level data collected from five study areas (Massachusetts, Connecticut, New Jersey and North Carolina and Florida) exposes regional variability due to glacial isostatic adjustment (GIA) of the solid Earth. In New Jersey, Massachusetts and Connecticut GIA corrected sea level was stable from at least BC 200 until AD 500. Sea level then increased at a rate of less than 1 mm/yr resulting from/associated with the Medieval Climate Anomaly. In North Carolina the rise in sea level began slightly later at AD 950. All records show stable or falling sea level between AD 1400 and the late 19th century at the time of the Little Ice Age. Since then, sea level has risen at greater than 2 mm/yr, representing the steepest century-scale increase of the past two millennia.