Could Sandy happen again? Maybe, says Tufts geologist

Public release date: 17-Oct-2013
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Contact: Katherine Cinnamond
Katherine.Cinnamond@tufts.edu
617-627-4703
Tufts University

Due to rising sea levels, smaller storms could produce significant flooding

MEDFORD/SOMERVILLE, Mass. Almost a year after Hurricane Sandy, parts of New York and New Jersey are still recovering from billions of dollars in flood damage. Tufts University geologist Andrew Kemp sees the possibility of damage from storms smaller than Sandy in the future.

"Rising sea levels exacerbate flooding," says Kemp. "As sea level rises, smaller and weaker storms will cause flood damage." An assistant professor in Tufts' Department of Earth and Ocean Sciences, Kemp co-authored a study on sea-level change close to New York that was published recently in the Journal of Quaternary Science.

Sandy hit New York as a team led by Kemp was researching sea-level change and flooding that had occurred in seven historically damaging hurricanes in New York since 1788. Last October, Sandy's storm surge hit the coast at high tide, but storm and tidal conditions were not the only cause of the devastation, Kemp says. Seawaters off New York's coast have risen 16 inches since 1778, the year of New York City's first major recorded storm, his research shows.

To make this determination Kemp and his team studied salt-marsh sediments from Barnegat Bay in northern New Jersey, south of the tide gauge at Battery Park in New York. Using sediment cores, long cylinders drilled into the marsh floor that offer scientists a look back through time, they were able to reconstruct sea-level changes since 1788.

Kemp cites two factors for rising seas. One is the natural sinking of land called glacio-isostatic adjustment. A second factor, and one supported by the latest report from the Intergovernmental Panel on Climate Change (IPCC), points to the melting of the ice-covered terrain of Greenland and Antarctic as well as the thermal expansion of ocean waters.

Looking forward, Kemp sees the possibility of storms less powerful than Sandy inflicting serious damage. He uses a basketball analogy. "It's like playing basketball and raising the level of the court so that shorter and shorter people can dunk. It makes low lying property and infrastructure more vulnerable at a time when developers are pumping money into coastal cities and towns."

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Tufts University, located on three Massachusetts campuses in Boston, Medford/Somerville, and Grafton, and in Talloires, France, is recognized among the premier research universities in the United States. Tufts enjoys a global reputation for academic excellence and for the preparation of students as leaders in a wide range of professions. A growing number of innovative teaching and research initiatives span all Tufts campuses, and collaboration among the faculty and students in the undergraduate, graduate, and professional programs across the university's schools is widely encouraged.

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Public release date: 17-Oct-2013
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| Share

]

Contact: Katherine Cinnamond
Katherine.Cinnamond@tufts.edu
617-627-4703
Tufts University

Due to rising sea levels, smaller storms could produce significant flooding

MEDFORD/SOMERVILLE, Mass. Almost a year after Hurricane Sandy, parts of New York and New Jersey are still recovering from billions of dollars in flood damage. Tufts University geologist Andrew Kemp sees the possibility of damage from storms smaller than Sandy in the future.

"Rising sea levels exacerbate flooding," says Kemp. "As sea level rises, smaller and weaker storms will cause flood damage." An assistant professor in Tufts' Department of Earth and Ocean Sciences, Kemp co-authored a study on sea-level change close to New York that was published recently in the Journal of Quaternary Science.

Sandy hit New York as a team led by Kemp was researching sea-level change and flooding that had occurred in seven historically damaging hurricanes in New York since 1788. Last October, Sandy's storm surge hit the coast at high tide, but storm and tidal conditions were not the only cause of the devastation, Kemp says. Seawaters off New York's coast have risen 16 inches since 1778, the year of New York City's first major recorded storm, his research shows.

To make this determination Kemp and his team studied salt-marsh sediments from Barnegat Bay in northern New Jersey, south of the tide gauge at Battery Park in New York. Using sediment cores, long cylinders drilled into the marsh floor that offer scientists a look back through time, they were able to reconstruct sea-level changes since 1788.

Kemp cites two factors for rising seas. One is the natural sinking of land called glacio-isostatic adjustment. A second factor, and one supported by the latest report from the Intergovernmental Panel on Climate Change (IPCC), points to the melting of the ice-covered terrain of Greenland and Antarctic as well as the thermal expansion of ocean waters.

Looking forward, Kemp sees the possibility of storms less powerful than Sandy inflicting serious damage. He uses a basketball analogy. "It's like playing basketball and raising the level of the court so that shorter and shorter people can dunk. It makes low lying property and infrastructure more vulnerable at a time when developers are pumping money into coastal cities and towns."

###

Tufts University, located on three Massachusetts campuses in Boston, Medford/Somerville, and Grafton, and in Talloires, France, is recognized among the premier research universities in the United States. Tufts enjoys a global reputation for academic excellence and for the preparation of students as leaders in a wide range of professions. A growing number of innovative teaching and research initiatives span all Tufts campuses, and collaboration among the faculty and students in the undergraduate, graduate, and professional programs across the university's schools is widely encouraged.

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AAAS and EurekAlert! are not responsible for the accuracy of news releases posted to EurekAlert! by contributing institutions or for the use of any information through the EurekAlert! system.

Source: http://www.eurekalert.org/pub_releases/2013-10/tu-cs101713.php
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