Sleet, Berks
- When
- March 17, 3:00 PM EST to March 18, 3:00 AM EST
- Where
- Berks forecast zone
- Reported by
- TRAINED SPOTTER
- Coordinates
- 40.416, -75.926 (the zone’s center; the record gives no point)
A wintry mix of snow, sleet, freezing rain and rain occurred across Eastern Pennsylvania from the afternoon of the 17th through the afternoon of the 18th. m.
Every event with a place to put it; 7 filed by county or forecast zone are drawn at its center, in a lighter ring. Tap one for its entry below.
Deaths and injuries are direct and indirect together, as the offices filed them. Damage is property and crops in the dollars of the year, not adjusted for inflation, and only where an office estimated it.
The episode as NWS PHI wrote it up.
A wintry mix of snow, sleet, freezing rain and rain occurred across Eastern Pennsylvania from the afternoon of the 17th through the afternoon of the 18th. In Philadelphia and its suburbs snow began falling between 3 p.m. EST and 4 p.m. EST on the 17th. Precipitation was mixed with some rain and sleet from the start in Philadelphia and Delaware Counties. After 8 p.m. EST precipitation fell as mainly rain with some sleet mixed in from time to time into the early morning of the 18th. Little accumulation occurred. Across Berks, Chester, Montgomery and Bucks Counties, the change to sleet and plain rain took longer. Mixed precipitation fell throughout the evening and there were even some pockets of freezing rain in the upper parts of the county. Precipitation fell as plain rain from the early morning on the 18th until it ended during that day. Snow and sleet accumulations averaged 0.5 to 3 inches. Across the Lehigh Valley, snow began falling between 3 p.m. EST and 5 p.m. EST on the 17th. Sleet began mixing in during the evening and mixed precipitation fell overnight. Plain rain occurred from around 5 a.m. EST onward on the 18th. Snowfall and sleet accumulations averaged around one inch as the heaviest precipitation remained south of the region. Across the Poconos, snow began falling between 4 p.m. and 6 p.m. EST on the 17th. Sleet, rain and freezing rain began mixing in with the snow after midnight EST on the 18th. The change to plain rain took most of the daylight hours on the 18th to go from the southern valleys in the early morning to the higher terrain in the mid-afternoon. Snow and sleet accumulations averaged around one inch as the heaviest precipitation remained south of the region. Ice accretions from the freezing rain were less than one-quarter of an inch. Since this event occurred on a Sunday night, no significant accidents were reported. High temperatures from the 14th through the 16th averaged in the 60s north and the 70s south. This probably helped keep road surfaces relatively warm and ice free throughout this event. Most of the accumulations reported were on grassy surfaces. Specific accumulations included 3.3 inches in Palm (Montgomery County), 2.8 inches in Newtown (Bucks County), 2.0 inches in Tobyhanna (Monroe County) and Warrington (Bucks County), 1.0 inch in Mount Pocono (Monroe County), Easton (Northampton County), Springtown (Bucks County), Hatfield (Montgomery County) and Doylestown (Bucks County), 0.9 inches in Albrightsville (Carbon County), 0.8 inches in Allentown (Lehigh County), 0.5 inches in East Stroudsburg (Monroe County) and Wynnewood (Montgomery County) and 0.2 inches in West Chester (Chester County). A strong cold front moved through the northeast on the 16th and brought in considerably colder air. A high pressure system built into eastern Canada and northern New England on the 17th and helped lock the cold air in place, especially at and within the lowest 5000 feet of our atmosphere. Meanwhile a weak low pressure system developed on the old cold frontal boundary in the Tennessee Valley during the morning of the 17th. It moved eastward off the Carolina coast on the18th. Because the low was so far south and weak, the heaviest precipitation remained from the Philadelphia suburbs and southern New Jersey southward with this event. On the other hand, since the low was relatively weak, so was the onshore flow and thus the longer it took to scour the cold air from the lower layers of the atmosphere.
The local office's own words before the first event, as it sent them, from the Iowa Environmental Mesonet's archive of National Weather Service text.
NWS Philadelphia/Mount Holly wrote its last area forecast discussion before the first event at Mar 17, 10:55 AM EST, 4 hours 5 minutes earlier.
AREA FORECAST DISCUSSION NATIONAL WEATHER SERVICE MOUNT HOLLY NJ 1055 AM EST SUN MAR 17 2002 ****************************************************************** LARGE ARCTIC HIGH OVR SE CANADA SENDING DOWN CHILLY NE-E WINDS. HAVE LWRD AFTN HIGHS A BIT. ALSO LWRD POPS. STEERING WINDS MOSTLY DUE E. N FA A BIT DRY CLOSEST TO HIGH...SO ANY PCPN TRYING TO INVADE THIS REGION WOULD BE MOSTLY VIRGA. HAVE KEPT FLURRIES FAR N...A MIX OF -RA/-SN FOR CENTRAL FA...AND PLAIN RAIN SOUTH AND ALONG THE COAST. ****************************************************************** A WET FCST IS IN STORE FOR THE REGION...LOTS OF HOURS OF PCPN BUT THE PCPN AMOUNTS ARE NOT EXPECTED TO BE HIGH ENOUGH TO PUT ANY KIND OF DENT INTO THE DROUGHT. PRECIPITABLE WATER INCR TO 3/4 TO ONE INCH BUT DYNAMICS ARE NOT ORGANIZED ENOUGH OVER THE FCST AREA...THEREFORE NO FCST OF HEAVY PCPN. CNVCTION DVLPG TENNESSEE IS HEADED NE WITH A SHORT WAVE EMBEDDED IN THE SW FLOW ALFT. THE MODELS BRING THIS SHRT WAVE INTO PA AT 18Z BUT LAG THE MOISTURE ASSOCIATED WITH IT. I THINK THE MODELS ARE TOO SLOW AND WILL TIME THE PCPN WITH THE SHORT WAVE AND GO FASTER THAN ANY MODEL SOLUTION SINCE PCPN IS DVLPG AND MOVING SO RAPIDLY FROM UPSTREAM. SINCE DYNAMIC OUTRUN THE MOISTURE...ANY PCPN WITH THIS SHOULD BE LIGHT. POPS GENLY CHC PHL NORTH AND LIKELY SOUTH. PER TYPE INTO EARL TNGT...THICKNESSES AND SOUNDINGS INDICATE ANY PCPN N AS SNOW. ACY-MIV-DOV ON SOUTH...RAIN. IN BETWEEN...THE MODEL SOUNDINGS (EXCEPT BELOW 1K FT) LEAN TWRD SNOW OVER RAIN. WITH THE BLYR WINDS FROM THE OCEAN WHERE WATER TEMPS ARE IN THE 40S THE TEMPS AT GROUND (DUE TO THIS FETCH) SHOULD BE HIGH ENOUGH TO MELT MOST ANY PCPN EVEN THOUGH IT WOULD INITIALLY FALL AS SNOW FROM ALFT. IF PCPN CAN DVLP AND GET HEAVY ENOUGH...THE COOLING EFFECT WOULD HELP TILT IN FAVOR OF SNOW. FOR NOW...THE WORDING IS RAIN OR SNOW N/W SUBURBS OF PHL AND CHC OF RAIN OR RAIN AND WET SNOW MIXED PHL AND S/E. THIS AFTN/S CONDITIONS CONTINUE INTO EARLY TNGT AND THEN THE ATMOSPHERE WARMS ENOUGH TO CHANGE MOST PCPN EXCEPT NORTH TO RAIN...THERE IT WARMS DURING MONDAY FOR A CHANGEOVER. LOW PRES FORMS ON THE FRONT TO THE SOUTH HELPING ENHANCE THE OVERRUNNING LATE TNGT AND MONDAY. WITH A WARM GROUND AND MARGINAL TEMPS FOR SNOW...ANY ACCUMULATIONS SHOULD BE SMALL AND CONFINED TO HIGHER ELEVATIONS NORTH. DIURNAL TEMPS WILL BE SMALL WITH CONTINUED OCEAN FETCH AND PCPN. MPO 37 28 36 32 / 40 80 80 20 ABE 39 31 38 35 / 40 90 90 20 RDG 39 32 38 35 / 40 90 90 20 PHL 43 36 42 41 / 50 100 100 20 12N 38 29 37 32 / 40 80 80 20 SMQ 43 34 40 38 / 50 100 100 20 TTN 43 34 40 38 / 50 100 100 20 MIV 44 37 43 42 / 60 100 100 20 ACY 42 38 43 42 / 60 100 100 20 ILG 43 36 42 41 / 50 100 100 20 DOV 44 37 43 42 / 60 100 100 20 GED 44 38 43 42 / 60 100 100 20 ESN 44 38 43 42 / 60 100 100 20 .PHI... DE...NONE. MD...NONE. NJ...NONE. PA...NONE. MARINE...SCA COAST AND LWR DEL BAY. RNS/WOODWORTH
The national radar mosaic for the moment the first event began.
10 sleet. Local standard time, as filed.
After NWS Directive 10-1605, the rules offices file Storm Data by.
Every storm in Pennsylvania in 2002Every state in 2002This day in weather historyWarnings in Pennsylvania, March 2002
NOAA National Centers for Environmental Information, Storm Events Database, compiled from the National Weather Service’s monthly Storm Data. Complete through 2026-06; NCEI adds each month about 75 days after it ends and revises past years a few times a year. Rebuilt 2026-09-24. Each event’s entry at NCEI: 5286469, 5286472, 5286473, 5286476, 5286478, 5286470, 5286474, 5286477, 5286471, 5286475.