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.