The beaches along the Eastern seaboard are about to disappear, says one EPA scientist. Why isn't anyone listening?
Posted Tuesday, April 27, 2010, at 10:02 AM
For most of the 20th century, Chesapeake Beach, Md., was known for its boardwalk, amusement park, and wide, sandy beaches, popular with daytrippers from Washington, D.C. "The bathing beach has a frontage of three miles," boasted a tourist brochure from about 1900, "and is equal, if not superior, to any beach on the Atlantic Coast."
Today, on a cloudless spring afternoon, the resort town's sweeping view of Chesapeake Bay is no less stunning. But there's no longer any beach in Chesapeake Beach. Where there once was sand, water now laps against a seven-foot-highwall of boulders protecting a strip of pricey homes marked with "No Trespassing" signs.
Surveying the armored shore, Jim Titus explains how the natural sinking of the shoreline and the slow but steady sea-level rise, mostly due to climate change, have driven the bay's water more than a foot higher over the past century. Reinforcing the eroding shore with a sea wall held the water back, but it also choked off the natural supply of sand that had replenished the beach. What sand remained gradually sank beneath the rising water.
Titus, the Environmental Protection Agency's resident expert on sea-level rise, first happened on Maryland's disappearing beaches 15 years ago while looking for a place to windsurf. "Having the name 'beach,' " he discovered, "is not a very good predictor of having a beach." Since then, he's kept an eye out for other beach towns that have lost their namesakes—Maryland's Masons Beach and Tolchester Beach, North Carolina's Pamlico Beach, and many more. (See a map of Maryland's phantom beach towns here.) A 54-year-old with a thick shock of hair and a sturdy build, Titus could pass for a vacationer in his Panama hat, khakis, and polo shirt. But as he picks his way over the rocky shore, he's anything but relaxed.
For nearly 30 years, Titus has been sounding the alarm about our rising oceans. Global warming is melting polar ice, adding to the volume of the oceans, as well as warming up seawater, causing it to expand. Most climatologists expect oceans around the world to rise between 1.5 feet and 5 feet this century. Some of the hardest-hit areas could be in our own backyard: Erosion and a shift in ocean currents could cause water to rise four feet or more along much of the East Coast. Titus, who contributed to the Intergovernmental Panel on Climate Change's Nobel Prize-winning 2007 report, has done more than anyone to determine how those rising seas will affect us and what can be done about them.
Like his occasional collaborator, NASA climatologist James Hansen, Titus has decided to speak out. He's crisscrossed the country to meet with state and local officials in coastal areas, urging them to start planning now for the slow-motion flood. Yet his warnings have mostly fallen on deaf ears. "We were often told by mid-level officials that their bosses did not want to plan for anything past the next election," he says.
Neither, it seems, does the federal government. Over the past decade, Titus and a team of contractors combined reams of data to construct a remarkably detailed modelof how sea-level rise will impact the eastern seaboard. It was the largest such study ever undertaken, and its findings were alarming: Over the next 90 years,1,000 square miles of inhabited land on the East Coast could be flooded, and most of the wetlands between Massachusetts and Florida could be lost.The favorably peer-reviewed study was scheduled for publication in early 2008 as part of a Bush administration report on sea-level rise, but it never saw the light of day—an omission criticized by the EPA's own scientific advisory committee. Titus has urged the more science-friendly Obama administration to publish his work, but, so far, it hasn't—and won't say why.
So Titus recently launched a personal Web site, Risingsea.net, to publish his work. "I decided to do my best to prevent the taxpayer investment from being wasted," he says. The site includes "When the North Pole Melts," a prescient holiday ditty recorded by his musical alter ego, Captain Sea Level, in the late '80s.
Titus gazes at Chesapeake Beach's jagged shoreline, where two children scramble over the barrier of large, gray boulders known as a revetment. "The children of 21st-century Chesapeake Beach, what do they do?" he asks. "They play on revetments." A generation ago, these kids might have been skipping through the waves. A generation from now, many of the rocks they're playing on will almost certainly be underwater.
Living near the ocean has always come with the risk of getting wet. Yet coastal dwellers whose homes got swamped by the occasional storm surge could rely on the water to recede eventually. That certainty is gone. Titus has calculated that a three-foot rise in sea level will push back East Coast shorelines an average of 300 to 600 feet in the next 90 years, threatening to submerge densely developed areas inhabited by some 3 million people, including large parts of New York City, Philadelphia, and Washington, D.C. As Margaret Davidson, director of the National Oceanic and Atmospheric Administration's Coastal Services Center in Charleston, South Carolina, puts it, "Today's flood is tomorrow's high tide."
The rising waters can be kept at bay by constructing dikes and bulkheads, pumping sand to fill out receding beaches, and elevating existing buildings and roads on embankmentsor pylons. But such efforts may prove prohibitively expensive—Titus says that in the lower 48 states alone, they could cost as much as $1 trillion over the next century, and he estimates that in the process, 60 percent to 90 percent of the East Coast's wetlands could be destroyed as bulkheads and other defensive measures restrict the movement of estuaries and marshes, drowning them when the ocean rises.
Josh Harkinson is a staff reporter at Mother Jones.
Kate Sheppard covers energy and environmental politics in Mother Jones' Washington bureau.
Photograph of wave by Jupiterimages/Getty Images.