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Rising waters threaten the coast of North Carolina

Climate change is carving its name into the state's retreating shorelines. Planners are taking official notice as they prepare for a wetter world.

By Bruce Henderson

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  • Rising waters threaten the coast of North Carolina
  • Rising waters threaten the coast of North Carolina
  • Rising waters threaten the coast of North Carolina
  • Officially 10 feet above sea level, the village of Swan Quarter is surrounded by fields, marshes and the lapping waters of Pamlico Sound.

    "You're in a part of the world where too much water is just as much a problem as too little water," said Rodney Woolard of the federal Natural Resources Conservation Service.

    After decades of battling floods and saltwater creeping up its network of drainage ditches, Swan Quarter won a $5.2 million stimulus grant to finish a 17-mile dike around the village and surrounding farmland.

    J.W. Spencer, chairman of the Hyde Soil and Water Conservation District board, estimates that over the years, thousands of acres of farmland have been taken out of use because of intruding saltwater.

    "It would completely sterilize the land," he said. "Grass won't even grow. It starts at the ditch and spreads over the land. You can take two months of saltwater and it can take 20 years to get it out."

    The water has risen since he was a kid, says Spencer, who is a Hyde native. But he attributes that to natural cycles.

    "I'm not disputing that we're not having some global warming, that the average temperature isn't a little more than it used to be and the sea a little higher," he said.

    "But we don't have the knowledge that it didn't happen 1,000 years ago. Or that in 300 years it won't be going back down again."

  • With 325 miles of oceanfront and 5,000 miles of shoreline around its seven sounds, North Carolina has one of the nation's most diverse coastlines. The Albemarle and Pamlico sounds form the second-largest estuarine system in the lower 48 states. They provide half the nursery grounds for all saltwater fish between Maine and Florida, and nurture most of the state's most economically important seafood. Commercial fishing brought in $77 million in 2009, while sport fishermen took home nearly 12 million pounds of fish. Coastal tourists spent $2.4 billion that year - more than a third of that on the vulnerable Outer Banks - and the industry employed 30,530 people. Almost $133 billion of coastal property is insured.

  • North Carolina is a late arrival to global warming.

    Last summer's heat, the warmest on record for the state, reflects an uptick in temperatures that began only in recent decades.

    Unlike much of the globe, state climatologist Ryan Boyles says, N.C. temperatures show no significant increase since reliable record keeping began in 1895.

    "The models suggest we should be warming, and we are not," he said. "We don't know why."

    State temperatures have gone up since the mid-1970s, as they have around the globe. Charlotte's three warmest years on record were in 1990, 1991 and 1998; six of its 19 hottest years have been logged since 1990. Average annual temperatures are up about 1 degree since 1981 compared to the previous 30 years.

    Duke University-led scientists recently linked climate change to intensified Bermuda Highs, the systems that bring hot, humid weather to the East in summer.

    But North Carolina's climate varies so much that no meaningful long-term trends in extreme temperatures, seasonal changes or frost dates emerge, Boyles says.

    Temperatures statewide also went up from 1910 to 1950, for example, then cooled.

    Overnight lows have gone up in recent decades, but Boyles attributes that to the heat-soaking concrete and asphalt of growing urban areas.

    While the state has suffered two devastating droughts since 2000, something similar struck between 1924 and 1934. Tree rings show that other dry spells in the past 1,000 years might have been even longer and drier.

    Hurricanes and tropical storms have smacked the N.C. coast hard since 1996, with 12 making landfall in the Southeast. That appears to be part of a natural upswing that typically lasts 25 to 30 years.

    Sea-level rise, however, "is closely linked to broader global warming," the State Climate Office says. Asheville's National Climatic Data Center says 2010 tied 2005 as the globe's warmest years on record.

  • Sea levels are measured both globally and locally.

    Global sea level was basically stable for the past 400 to 2,000 years, says the U.S. Climate Change Science Program. Between 1900 and 2000, it rose by an average rate of 6.7 inches a century. Between 1993 and 2003, the rate rose to 12.2 inches a century, although that could be partly due to natural fluctuations.

    Relative sea level factors in local conditions, such as the tides, currents, changes in the sea floor and sinking land. It varies from place to place along the same coastline: Levels are going up 16.8 inches a century in Duck, on the northern coast, but just 8.4 inches south in Wilmington.

MANNS HARBOR The sea that sculpted North Carolina's coast, from its arc of barrier islands to the vast, nurturing sounds, is reshaping it once again.

Water is rising three times faster on the N.C. coast than it did a century ago as warming oceans expand and land ice melts, recent research has found. It's the beginning of what a N.C. science panel expects will be a 1-meter increase by 2100.

Rising sea level is the clearest signal of climate change in North Carolina. Few places in the United States stand to be more transformed.

About 2,000 square miles of our low, flat coast, an area nearly four times the size of Mecklenburg County, is 1 meter (about 39 inches) or less above water.

At risk are more than 30,500 homes and other buildings, including some of the state's most expensive real estate. Economists say $6.9 billion in property, in just the four counties they studied, will be at risk from rising seas by late this century.

Climate models predict intensifying storms that could add billions of dollars more in losses to tourism, farming and other businesses.

While polls show growing public skepticism of global warming, the people paid to worry about the future - engineers, planners, insurance companies - are already bracing for a wetter world.

"Sea-level rise is happening now. This is not a projection of something that will happen in the future if climate continues to change," said geologist Rob Young of Western Carolina University, who studies developed shorelines.

Nobody knows how high or fast the sea will rise. Water isn't likely to submerge all the state's low coastland because landowners will fight back. But the coast we know, with its fringe of salt marshes, its fluffy beaches and old harbor towns, might look like a different place a few generations from now.

That won't be the work of rising water alone, but of quirks in North Carolina's coastal topography. The flat ground means even a small increase in water level will spread far inland. The coastal plain is also sinking, the geologic legacy of the last Ice Age.

Sea-level rise magnifies two other powerful forces - erosion that gouges the coastline and the pounding of nor'easters and tropical storms.

Storms, Young said, are "the hammer" of rising seas. As storm surges pound ashore on a higher base of water, their damage multiplies.

The Outer Banks, some scientists predict, could disintegrate into a string of high spots - Avon, Buxton, Ocracoke - reachable only by boat.

If storms punch new inlets through the islands, the brackish sounds and wetlands that serve as vital nurseries for Atlantic coast seafood species would turn into open saltwater. Predatory fish would pour into previously protected waters. Marshes would migrate inland or drown.

Dead bald cypress trees already rim the Albemarle-Pamlico Peninsula, graying in the encroaching salty water that engulfed and killed them. Much of the peninsula, which juts toward the northern Banks and is one the state's richest wildlife sanctuaries, could be underwater by century's end.

Human habitats will be forced into momentous decisions - fortify or flee.

A row of beach houses in the old resort town of Nags Head is collapsing into the surf now as the town plans a $36 million project to pump fresh sand onto its eroding strand this spring. Down the coast, in North Topsail Beach, property owners are waffling on helping to pay for a $10 million nourishment project.

As sand moves around, some beaches such as Sunset actually widen. But communities that control about a third of the state's 325 miles of beach face similar sink-or-swim decisions. The average cost of pumping sand onto eroding beaches is nearly $1 million per mile, repeated about every five years as storms wash it away.

One coastal village repeatedly swamped by storms is barricading itself, Dutch-style, behind a 17-mile dike.

State planners are preparing detailed maps of future high-water lines, groundwork for an eventual retreat inland of both people and buildings.

"To me, it's the big planning problem for this century," said Scott Shuford, planning director in Onslow County, on the southern coast. "There's an element of urgency about it, but at the same time a recognition that it can't be solved easily."

Drafting sea-level policy

It seems implausible that an almost imperceptible rise in the sea - about the thickness of two nickels a year - could cause such havoc.

But it took only an 8-inch global rise to threaten the iconic Cape Hatteras Lighthouse, which was 1,500 feet from the Atlantic when it was built in 1870. By 1999, when hydraulic jacks gingerly nudged the striped brick tower inland, waves crashed at its foundation.

Long before people were capable of such engineering, the sea and wind were shaping the Carolina coast. After the last Ice Age peaked 11,000 years ago, melting glaciers turned Pamlico Creek into Pamlico Bay, then into Pamlico Sound.

Coastal geologists who reconstructed sea-level changes on the northeastern N.C. coast say levels were stable for 3,000 years. The sea began rising in the 19th century. The rate of climb doubled again in the 20th century, with a further quickening in the past 30 years.

Alonzo Leary gauges the changes over the 74-year span of his life. Raised near Albemarle Sound in a farming community called Alligator, he left as a young man to find work. He returned 20 years later to find old swimming holes flooded and the sound closer to road level.

"I notice that the swamps stay full of water most of the time," Leary said.

Scientists envision more acceleration this century. Some say seas could rise to as much as 6 feet above current levels by 2100 if large ice masses melt in Greenland and Antarctica.

Because the stakes are so high, local and state policy leaders are paying new attention to sea-level rise.

To help plan for building new roads, bridges and other infrastructure, a state panel of engineers and scientists recommended estimates last year that the sea will rise 15 to 55 inches by 2100, with 39 inches, or 1 meter, the midpoint.

The N.C. Division of Coastal Management is circulating drafts of what could become the state's first policy on sea-level rise. If adopted, the policy would lay the groundwork for regulations influencing development and how public structures from boat ramps to bridges are built.

When state transportation engineer Ted Devens and his colleagues recently designed a 28-mile widening of U.S. 64 across the Albemarle-Pamlico Peninsula, they raised the roadbed by a foot to allow for rising seas. It was a first for an N.C. Department of Transportation road project.

"What we're trying to do is get away from the hype and just look at the data," said Devens, who works in project development and environmental analysis. "Our data tells us sea level is rising.

"What do you plan for? That's been the big question."

Armed with a $5 million federal grant, state planners are using high-resolution flood-plain maps and geologic data to assess future flood risks from higher seas and storms, and how to respond.

At some tipping point - state officials calculate sea-level rise will cause significant problems by about 2042 - decisions will have to be made. Infrastructure such as water and sewer lines, and industries, will have to be moved inland.

"Do you move those things now or do you wait? It gets to be an interesting chicken-and-egg question," said study leader John Dorman of the state flood-plain mapping program.

Other key questions: where to move both structures and people, and how to pay for it?

In the little town of Plymouth, where the Roanoke River flows into Albemarle Sound, storms regularly submerge the century-old sewage system, once stranding a town employee at the treatment plant. It will only get worse as water in the sound rises.

"Everybody's going to have to start figuring, where do we go from here?" said Mayor Brian Roth. "We know that we're going to have to deal with these issues. These small towns cannot possibly handle the money this is going to take, no way."

Rob Young, the coastal geologist, credits the state's planning efforts. But if the state were serious about adapting to rising seas, he says, it would be smarter in responding to the storms that already hammer the coast.

Beach communities shredded by hurricanes are typically built back, sometimes repeatedly. Taxpayers subsidize federal flood insurance, roads and bridges.

If seas rise by 1 meter, Young said, engineers could fix the holes storms would blow through the rim of barrier islands, as long as the state can afford repairs. The problem of the future is that Charleston, Miami and other East coast cities also would be struggling to keep their heads above water.

"If we have to fix Manhattan," he said, "Hatteras is not going to compete for money real well."

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