Sea level in Northeastern US rising more than three times faster than global average
As the world warms and seas rise, some spots are expected to take the brunt of the higher ocean levels, while others may not see such a deluge, new research by the U.S. Geological Survey (USGS) reveals.
The study homed in on one "hotspot," where sea levels are rising more than three times faster than the global average: the 621-mile (1,000-kilometer) stretch along the eastern United States' Atlantic coast.
From Cape Hatteras, N.C., to north of Boston, Mass., tide-gauge records reveal sea levels have increased on average about 0.08 inches (2 millimeters) per year from 1950 to 2009. Globally, meanwhile, sea levels have increased about 0.02 inches (0.6 millimeter) per year during that window.
Records for a more recent, 40-year period, beginning in 1970, revealed faster rates of sea-level rise both globally and for this stretch of the U.S. East Coast. And rates are expected to continue increasing as global warming, which climate scientists agree is the result of greenhouse gas emissions, continues.
Researchers expected this to have a direct impact on people living in this area.
"Cities in the hotspot, like Norfolk, New York and Boston already experience damaging floods during relatively low-intensity storms," lead researcher Asbury Sallenger with the USGS said in a statement. "Ongoing accelerated sea-level rise in the hotspot will make coastal cities and surrounding areas increasingly vulnerable to flooding by adding to the height that storm surge and breaking waves reach on the coast."
Sea-level rise is primarily driven by two factors. Melting ice, from mountain glaciers to ice sheets, is an important contributor. Ultimately, the ice sheets that cover Greenland and Antarctica are expected to make massive contributions. Warmth also causes water to take up more space, a phenomenon called thermal expansion. [Stunning Photos of Antarctic Ice]
But the effects don't play out evenly everywhere for a number of reasons. For instance, melting ice can cause land to rebound as weight is lifted, causing relative sea level to fall. Melting ice redistributes mass on the planet, and as a result, changes the distribution of the oceans. Likewise, changes in currents and winds alter the distribution of ocean-expanding heat.
The research team links rapid sea-level rise within this hotspot to a slowdown in the Atlantic Meridional Overturning Current, which transports warm water from the tropics into the higher latitudes. Fluctuations in this current have profound implications for climate, according to the U.S. National Oceanic and Atmospheric Administration.
The results of the research were detailed in Sunday's (June 24) issue of the journal Climate Change.
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