Sea Level Rise to Affect NYC, Northeast Most

Michael Reilly, Discovery News
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March 16, 2009 -- Not far off the east coast of the United States, a mountain of water is lurking. If even a moderate amount of global warming takes place in the next century, a new study says it could slosh toward shore, doubling the rate of sea level rise in New York City.

Predictions on how much the oceans will rise by 2100 are highly uncertain; the latest estimates range from 50 centimeters to over a meter (1.6 to 3.3 feet). Melting glaciers play a large role in those estimates, as do rising temperatures, which cause ocean waters to swell as they trap heat.

The eastern seaboard of the United States is experiencing a bit of good sea level luck right now; waters in the area are around 0.6 meters (2 feet) lower than the global average. The trough is maintained by the Gulf Stream and North Atlantic Current, two powerful mid-ocean rivers that pile water up offshore as they course north toward the chilly latitudes of the Arctic.

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But Jianjun Yin of Florida State University and a team of researchers wondered what will happen to water levels if climate change weakens the currents as expected. Warming ocean temperatures and increased freshwater precipitation are expected to disrupt circulation in the Atlantic by as much as 30 percent, even when ignoring the potential for melting glaciers exacerbating the effect.

"Right now the currents are just offshore, but if they decline it will cause rapid sea level rise," Yin said.

Excluding the effects of ice sheet melting on sea level, the team estimates global waters will swell 21, 26 and 28 centimeters for scenarios of low, medium and high warming. Shifting currents could pile on an additional 15, 20, and 21 centimeters for the northeastern United States. New York City and Boston and most of the northeast are likely to be hit the hardest.

The effect becomes greater when the full scope of the world's melting ice is considered. The team's work was published yesterday in the journal Nature Geoscience.


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