A new study can confirm that Atlantic City and other areas of southern New Jersey will one day be submerged by rising sea levels.
A team led by Rutgers University determined that sea levels along the east coast of the US rose faster in the 20th century than in the last 2,000 years – with the fastest rise in the Garden State.
Researchers analyzed levels at six locations in Connecticut, New York City, New Jersey and North Carolina, and revealed that the locations experienced a total of 1.4 inches of sea level rise from 1900 to 2000.
However, southern New Jersey had the highest rates at about 0.63 inches per decade in some areas and 0.6 inches in others.
The spike in sea level is contributed to melting ice and warming of the oceans due to climate change, according to researchers.
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Scientists have long speculated that Atlantic City and other areas of southern New Jersey will one day be submerged by rising sea levels, and a new study can confirm this claim. Pictured is Edwin B. Forsythe National Wildlife Refuge in New Jersey showing how sea levels have risen
“The study looked for the first time at the phenomena that contributed to sea level change over 2,000 years at six locations along the coast, using a sea level budget,” the team shared in a statement.
Researchers chose to use a seal level budget, which increases understanding of the processes that drive sea level change.
The processes are global, regional (including geological, such as subsidence) and local, such as groundwater extraction.
Jennifer S. Walker, a postdoctoral fellow in the Department of Earth and Planetary Sciences at the School of Arts and Sciences at Rutgers University-New Brunswick, said: necessary for regional and local planning and responding to future sea level rise. ‘

Researchers analyzed levels at six locations in Connecticut, New York City, New Jersey and North Carolina, and revealed that the locations experienced a total of 1.4 inches of sea level rise from 1900 to 2000.
‘By learning how different processes vary over time and contribute to changes at sea level, we can more accurately estimate future contributions at specific locations.’
Climate change has become a major concern among the scientific community in recent years, which has also pushed their eyes to low-lying islands, cities and countries.
With melting glaciers and warming oceans, sea levels make such locations more vulnerable to flooding and storm damage.
The Great Hurricane of 1938 plowed through New England, devouring Long Island and Connecticut.
The storm, considered the worst in New England history, left 564 dead, injured more than 1,700 and destroyed some 15,000 infrastructure.
A more recent event occurred in 2012 when Hurricane Sandy swept through southern New Jersey and up to Long Island, New York, leaving nothing but destruction in its path.
It caused $ 70 billion in damage, cut the power of 8.5 million Americans, and destroyed about 650,000 homes.
And scientists link these devastating events to rising sea levels.
Most sea-level budget studies are global and, according to the recent study, are limited to the 20th and 21st centuries.
Researchers led by Rutgers estimate budgets at sea level for longer time frames of more than 2,000 years.
“The goal was to better understand how the processes that drive sea level have changed and may affect future changes, and this sea level budgeting method could be applied in other locations around the world.”


A recent event occurred in 2012 when Hurricane Sandy swept through southern New Jersey and up to Long Island, New York, leaving nothing but destruction in its path. Depicted is the aftermath of Superstorm Sandy in Atlantic City


Using a statistical model, scientists developed sea level budgets for six locations, splitting sea level records into global, regional and local components. They found that regional subsidence – the sinking of the land since the Laurentide Ice Sheet retreated thousands of years ago – has dominated each site’s budget for the past 2,000 years.
Using a statistical model, scientists developed sea level budgets for six locations, splitting sea level records into global, regional and local components.
They found that regional subsidence – the sinking of the land since the Laurentide Ice Sheet retreated thousands of years ago – dominates any site’s budget over the past 2,000 years.
Other regional factors, such as ocean dynamics, and site-specific local processes, such as groundwater abstraction causing land to sink, contribute much less to any budget and vary over time and by location.