NWSFO Boston (Taunton), Massachusetts, CWA — The storm produced up to 29 inches
of snow, blizzard conditions, and a (relatively minor) 2-foot storm surge along the coast.
Over 20 inches of snow fell in Rhode Island, Connecticut, and Plymouth and Bristol Counties
in Massachusetts. This swath was a continuation of the heaviest snow band which originated
in central Virginia, then crossed eastern Pennsylvania and northeast New Jersey. The
snowfall from this storm added to the existing snow cover, giving Boston's Logan Airport 30
inches on the ground. This broke the all-time snow depth record of 29 inches set in February
1978. However, the 18.2 inch total for this storm at Logan was only the seventh heaviest
snowfall event—the Blizzard of '78 is this area's benchmark storm.
The storm's main impact was to shut down school systems, airports, and other transportation
means for several days. In addition, heavy snow accumulations collapsed roofs in the days
following the blizzard.
Southern New England
Southern New England was also on the northern fringes of this event. All available model
guidance indicated a sharp gradient of the Quantitative Precipitation Forecast (QPF) and relative
humidity fields. Due to model interpretation and the uncertainty of the guidance, warning and
watch lead times were somewhat reduced for a large section of the CWA. Nonetheless, NWSFO
Taunton issued numerous statements to update the situation. A Winter Storm Watch was issued
Saturday morning at 0900 UTC, January 6, for the possibility of heavy snow for Cape Cod, the
Islands, and south coastal Rhode Island. At 0900 UTC, January 7, a second period Winter Storm
Warning was issued for the entire Taunton CWA except for Franklin and Hampshire Counties in
Massachusetts and Cheshire and Hillsborough Counties in New Hampshire. At that time, these
counties were covered with a Winter Storm Watch. In the January 7 afternoon forecast package,
all of the Taunton CWA was placed under a Winter Storm Warning. By 0200 UTC, January 8,
southeast coastal Massachusetts, including the city of Boston, and south coastal Rhode Island
were upgraded to a Blizzard Warning.
As model guidance shifted the snow northward across Massachusetts with time, the Boston
forecasters had to catch up to the event and issue warnings instead of watches. Post-storm
reviews by the Taunton office noted that the areal extent of the watch should have been increased
according to the conservative Eastern Region policy of issuing watches when the probability of
the event occurring is at least 30 but less than 70 percent.
Like many notable winter storms, portions of the southern New England coastline were
threatened with storm surge flooding. A Coastal Flood Watch was issued early on the morning of
January 7 and upgraded to a Coastal Flood Warning that afternoon. The tide of concern was the
afternoon high tide of January 8. Just before high tide, the wind became northerly and parallel to
the immediate coast, lessening the threat for coastal flooding. Consequently, the impact was
relatively minor with some flooding of shore roads, a few of which were closed for a short time.
The NWSFO in Taunton continued coordinating with external users in southern New England
even though the storm was initially forecast to head out to sea south and east of the area. As the
storm track changed, this constant contact proved beneficial because emergency managers were
kept briefed and well informed. After additional coordination calls, the Massachusetts Emergency
Management Agency opened on Sunday and the mayor of Boston ordered the removal of existing
snow on city streets prior to the onset of the storm.
Mead Herrick, Director of the New Hampshire Emergency Management Agency, was
satisfied with the level of service provided by NWS offices but stressed that this was not of the
same magnitude that it was farther south. For this area of the country, this was a winter storm
and not a blizzard. He felt the coordinating office was well in tune with this, and the forecast
products and coordination were in keeping with the event.