After the nor’easter, a canceled flood warning still left local tide alerts
The National Weather Service canceled coastal flood warnings on September 27, but narrower advisories and statements continued into September 28. The change marked a lower forecast hazard in specific zones, not a finding that every waterfront road or basement was safe.

A coastal flood warning can end while a shoreline still faces high-tide water. That is what the National Weather Service’s September 27 updates showed around New York City and northern New Jersey: the earlier warning was canceled, then lower-level advisories or statements identified particular places and hours of remaining risk. Reading the cancellation alone would miss the second half of the message. These were forecasts issued during the storm, not a current alert for September 29.
At 3:14 p.m. Eastern time on September 27, the weather service replaced the warning for the Bronx, northern Queens, northern Nassau and northwestern Suffolk with an advisory running from 10 p.m. Sunday to 2 p.m. Monday. It projected one to one and a half feet of water above ground in vulnerable shoreline locations, locally two feet, with the highest levels likely at Monday morning’s high tide. That forecast was lower than the earlier warning’s expectation of as much as three feet in vulnerable areas. The words “warning canceled” therefore described a change in severity and timing, not a withdrawal of every tide-related hazard.
The replacement was not uniform across the city. For Brooklyn, the weather service issued a coastal flood statement for Sunday evening through Monday morning, projecting one foot or less of inundation in vulnerable waterfront places. Southern Queens received an advisory projecting one to one and a half feet. For Manhattan and Staten Island, a statement covered the same overnight-to-morning period. A resident checking only a broad “New York City” headline could overlook that an advisory, a statement and their end times differed by county and shoreline.
Notify NYC translated that zone-by-zone forecast into local notices. Its September 27 afternoon advisory identified northern Queens and the Bronx from 10 p.m. to 2 p.m. Monday, while a separate statement covered Staten Island, Manhattan and Brooklyn from 7 p.m. to noon. The city warned against walking or driving through floodwater, advised moving vehicles from exposed places and directed residents to report impassable roads or property damage through 311. Those instructions concerned practical exposure even under a reduced alert category; they did not say that flooding occurred at every place named in a forecast.
Across the Hudson, a weather service statement for Hudson, eastern Bergen, eastern Essex and eastern Union counties likewise followed cancellation of a warning. It projected one foot or less of inundation at the most vulnerable waterfront sites from Sunday evening through Monday morning. Farther south, the Mount Holly forecast office’s Monday discussion said the storm was slowly departing and the coastal flooding threat had eased in many areas, while back bays in New Jersey and Delaware remained a concern. The office added advisories for Atlantic and Cape May counties. A falling regional threat and a new local advisory can coexist because tidal geography and the timing of high water differ.
The distinction also matters for evaluating government action. New Jersey’s September 25 state-of-emergency order covered eight counties and activated coordination among state and county agencies ahead of the storm. A weather-service warning’s cancellation is not, by itself, evidence that this separate legal declaration ended; the order and the weather alerts are different instruments. Residents and travelers needed to follow the relevant local update for their route or property rather than infer one statewide condition from a single canceled product.
This account compares dated public forecasts and city notices, not measured inundation at individual homes, casualty totals or a final damage survey. It does not establish that every forecast level materialized. The useful lesson from the September 27 transition is narrower: check the named zone, the replacement product, its effective hours and the next high tide before interpreting the word “canceled.” The accompanying image is a generated illustration of coastal-flood mechanics, not a photograph of the storm or an observed New York or New Jersey street.
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