The Perfect Storm

THE DREAMS OF THE DEAD

All collapsed, and the great shroud of the sea rolled on as it had five thousand years ago.

—HERMAN MELVILLE, Moby Dick

BY the time word has spread throughout Gloucester that the fleet’s in trouble, the storm has retrograded to within 350 miles of Cape Cod and developed such a steep pressure gradient that an eye starts to form. Satellite photos show a cyclonic swirl two thousand miles wide off the East Coast; the southern edge reaches Jamaica and the northern edge reaches the coast of Labrador. In all, three quarters of a million square miles of ocean are experiencing gale-force conditions, and an area three or four times that is indirectly involved in the storm. On the satellite photos, moist air flowing into the low looks like a swirl of cream in a cup of black coffee. Thick strands of white cloud-cover and dark Arctic air circle one-and-a-half times around the low before making it into the center. The low grinds steadily toward the coast, intensifying as it goes, and by the morning of October 30th it has stalled two hundred miles south of Montauk, Long Island. The worst winds, in the northeast quadrant, are getting dragged straight across Gloucester Harbor and Massachusetts Bay.

So sudden and violent are the storm’s first caresses of the coast that a tinge of hysteria creeps into the local weather bulletins: UNCONFIRMED REPORTS OF TWO HOUSES COLLAPSING HAVE BEEN RECEIVED FROM THE GLOUCESTER AREA … OTHER MASSACHUSETTS LOCATIONS UNDER THE GUN … SEAS OF 25 TO 45 FEET HAVE OCCURRED TODAY FROM GEORGES BANK EAST … THE DANGEROUS STORM ASSOCIATED WITH HIGH SEAS IS MOVING CLOSER TO NEW ENGLAND.

The first coastal flood warnings are issued at 3:15 AM on the 29th, based mainly on reports from Nantucket of sustained winds up to forty-five knots. Predictions from the Weather Service’s computers are systematically exceeding almost all atmospheric models for the area, and high tides are predicted to be two to three feet above normal. (These predictions, as it turns out, will be way too low.) The warnings go out via satellite uplink along something called the NOAA Weather Wire, which feeds into local media and emergency services. By dawn, radio and television announcers are informing the public about the oncoming storm, and the state Emergency Management Agency is contacting local authorities along the coast to make sure they take precautions. The EMA is based in Framingham, Massachusetts, outside of Boston, and has direct lines to Governor Weld’s Office, the National Guard, the State Police barracks, and the National Weather Service. Any threat to the public health is routed through the EMA. If local communities don’t have the resources to cope, state agencies step in; if state agencies can’t handle it, the federal government gets called. The EMA is set up to handle everything from severe thunderstorms to nuclear war.

October 30th, on shore, starts deceptively calm and mild; oak leaves skitter down the street and the midday sun has a thin warmth to it that people won’t feel again until spring. The only sign that something is amiss is along the coast, where huge grey swells start to roll in that can be heard miles inland. Swells are the outriders of sea weather, and if they keep getting bigger, the weather is approaching. The Gloucester Police Department blocks access to the shore but people go anyway, parking their cars half a mile away and walking through the rising wind and rain to hilltops where they can look out to sea. They are greeted by an ocean that has been wholly transformed. Swells march shoreward from the horizon in great, even bands, their white crests streaming sideways in the wind and their ranks breaking, reforming, and breaking again as they close in on Cape Ann. In the shallows they draw themselves up, hesitate, and then implode against the rocks with a force that seems to shake the entire peninsula. Air trapped inside their grey barrels gets blown out the back walls in geysers higher than the waves themselves. Thirty-foot seas are rolling in from the North Atlantic and attacking the town of Gloucester with a cold, heavy rage.

By midafternoon the wind is hitting hurricane force and people are having a hard time walking, standing up, being heard. Moans emanate from the electric lines that only offshore fishermen have ever heard before. Waves inundate Good Harbor Beach and the parking lot in front of the Stop-n-Shop. They rip up entire sections of Atlantic Road. They deposit a fifteen-foot-high tangle of lobster traps and sea muck at the end of Grapevine Road. They fill the swimming pool of a Back Shore mansion with ocean-bottom rubble. They suck beach cobbles up their huge faces and sling them inland, smashing windows, peppering lawns. They overrun the sea wall at Brace Cove, spill into Niles Pond, and continue into the woods beyond. For a brief while it’s possible to surf across people’s lawns. So much salt water gets pumped into Niles Pond that it overflows and cuts Eastern Point in half. Eastern Point is where the rich live, and by nightfall the ocean is two feet deep in some of the nicest living rooms in the state.

In several places around the state, houses float off their foundations and out to sea. Waves break through a thirty-foot sand dune at Ballston Beach in Truro and flood the headwaters of the Pamet River. Six-thousand-pound boat moorings drag inside Chatham Harbor. The Pilgrim Nuclear Power Plant in Plymouth shuts down because seaweed clogs the condenser intakes. A Delta Airlines pilot at Logan is surprised to see spray from breaking waves top the 200-foot cranes on Deer Island; just sitting on the runway, his airspeed indicator clocks eighty miles an hour. Houses are washed out to sea in Gloucester, Swampscott, and on Cape Cod. Rising waters inundate half of the town of Nantucket. A man is swept off the rocks in Point Judith, Rhode Island, and is never seen again, and a surfer dies trying to ride twenty-foot shorebreak in Massachusetts. Plum Island is cut in half by the waves, as is Hough’s Neck and Squantum, in Quincy. Over one hundred houses are destroyed in the town of Scituate, and the National Guard has to be called out to help the inhabitants evacuate. One elderly woman is taken from her house by a backhoe while surf breaks down her front door.

The winds have set so much water in motion that the ocean gets piled up against the continent and starts blocking the rivers. The Hudson backs up one hundred miles to Albany and causes flooding, and the Potomac does the same. Tides are five feet above normal in Boston Harbor, within one inch of an all-time Boston record. Had the storm occurred a week earlier, during the highest tides of the month, water levels would be a foot and a half higher, flooding downtown Boston. Storm surge and huge seas extinguish Isle of Shoals and Boone’s Island lighthouses off the coast of Maine. Some Democrats are cheered to see waves obliterate the front of President Bush’s summer mansion in Kennebunkport. Damage along the East Coast surpasses one and a half billion dollars, including millions of dollars in lobster pots and other fixed fishing gear.

“The only light I can shed on the severity of the storm is that until then, we had never—ever—had a lobster trap move offshore,” says Bob Brown. “Some were moved thirteen miles to the west. It was the worst storm I have ever heard of, or experienced.”

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BY nightfall on the 30th—with wave heights at their peak and the East Coast bearing the full brunt of the storm—the Coast Guard finds itself with two major search-and-rescue operations on its hands. In Boston, a Coast Guardsman starts telephoning every harbormaster in New England, asking if the Andrea Gail is in port. If the town is too small to have a harbormaster, they ask a town selectman to walk down to the waterfront and take a look. Coast Guard cutters also poke their way along the coast checking every harbor and cove they can find. In Maine’s Jonesport area a cutter checks Sawyers Cove, Roque Harbor, Black Cove, Moose Peak Light, Chandler and Englishman Bay, Little Machias Bay, Machias Bay East Side, Machias Bay West Side, and Mistaken Harbor, all without success. The entire coast from Lubec, Maine, to eastern Long Island is scrutinized without turning up any sign of the Andrea Gail

The search for Rick Smith is in some ways simpler than for the Andrea Gail because the pilots know exactly where he went down, but a single human being—even with a strobe light—is extremely hard to spot in such conditions. (One pilot missed a five-hundred-foot freighter because it was obscured by waves during one leg of his search.) As a result, the combined assets of half a dozen East Coast airbases are thrown into the search. Smith has a wife and three daughters at home and he knows, personally, a significant proportion of the people who are looking for him. He’s one of the most highly trained survival swimmers in the world and if he hits the water alive, he’ll probably stay that way. He might eventually die of thirst, but he’s not going to drown.

The first thing the Coast Guard does is drop a radio marker buoy where the other Guardsmen were picked up; the buoy drifts the way a person would, and the search area shifts continuously southwestward. Planes fly thirty- mile trackline searches five hundred feet above the water, but in these conditions the chances of spotting a man are