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Syracuse Lake Effect Snow

Why Lake Ontario buries Syracuse, what NOAA's 1991-2020 normals show, and every active NWS winter product, as issued.

Season normal: 127.8 inches at SYRACUSE HANCOCK INTL AP, NY US
Seasonal snowfall normal
128 in
Snowiest month
January
The lake
Lake Ontario

Syracuse snowfall, by the numbers

NOAA NCEI normals, 1991-2020
127.8 in
seasonal normal
SYRACUSE HANCOCK INTL AP, NY US
34.0 in
in January alone
the peak month
Nov to Apr
months with 1 in or more
the season window
Lake Ontario
the engine
NY snowbelt

Every figure is NOAA NCEI’s official 1991-2020 climate normal for the named station, SYRACUSE HANCOCK INTL AP, NY US (USW00014771). Lake effect gradients are sharp: a few miles can change a season total by feet.

The calendar

Month by month snowfall in Syracuse

NOAA’s 1991-2020 monthly snowfall normals for SYRACUSE HANCOCK INTL AP, NY US, laid out as a snow season from July to June. Lake effect climates load their totals into the cold months when the lake is still open water; watch how fast the bars rise in November and fall off late winter.

Monthly snowfall normals (inches), SYRACUSE HANCOCK INTL AP, NY US, NOAA NCEI 1991-2020 U.S. Climate Normals.
Satellite view of parallel lake effect snow bands streaming southeast off all five Great Lakes
Lake effect snow bands streaming off the Great Lakes, in a NOAA satellite view. Cold air crossing warm water organizes into these parallel cloud streets, and where one comes ashore it snows hard while the next town over sees sun. “Lake effect snow bands over the Great Lakes region” — NOAA — Public domain
The mechanism

Why Syracuse gets lake effect snow

Syracuse catches lake effect bands that form over Lake Ontario on a west-northwest flow and ride southeast across Oswego County into Onondaga. Add the nor'easters that run up the eastern seaboard and Syracuse routinely posts the highest seasonal snowfall of any large US city, a title the privately run Golden Snowball and Golden Snow Globe contests track with civic glee.

The physics, in the National Weather Service’s own words: “Lake Effect snow occurs when cold air, often originating from Canada, moves across the open waters of the Great Lakes... The air rises, clouds form and grow into narrow band that produces 2 to 3 inches of snow per hour or more.” And on location: “Wind direction is a key component in determining which areas will receive lake effect snow. Heavy snow may be falling in one location, while the sun may be shining just a mile or two away in either direction.” (NWS, What is Lake Effect Snow?)

Satellite view of snow covered snowbelts downwind of Lake Erie and Lake Ontario with both lakes open
Lake Erie, Lake Ontario and their snowbelts from NASA's MODIS, January 13, 2017. The white land downwind of each lake is the belt itself: snow drawn on the map by fetch and wind direction. “Lake Erie, Lake Ontario, and the Finger Lakes” — Jeff Schmaltz, MODIS Land Rapid Response Team, NASA GSFC — Public domain
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Live, as issued

Winter weather products covering NY right now

Every active National Weather Service winter product for New York, read live from api.weather.gov and reproduced exactly as issued. Zones are larger than the city, so confirm the listed areas include yours.

Checking api.weather.gov for active winter weather products…

Why the mixed product names: for the 2017-2018 winter the NWS consolidated its lake effect products into the general winter suite. The Lake Effect Snow Warning came back on October 1, 2019, but per Service Change Notice 19-63 its use is “optional at Regional discretion” and offices may still issue Winter Storm Warnings “with the lake effect component specified in the ‘What’ section”. The old Lake Effect Snow Watch and Advisory were never reinstated. So this page passes through every winter product for the area and tags the ones whose own NWS text names lake effect.

Whiteout and travel decisions belong with the National Weather Service (weather.gov winter safety) and the New York 511 system (511 road conditions). NWS products above are reproduced as issued.

The season

When lake effect season runs, and what ends it

Lake effect season opens with the first arctic outbreaks over still-warm water, usually November, and the early-season events are often the most violent because the lake is warmest. What closes the season depends on the lake: shallow Lake Erie usually freezes and shuts its machine off, while deep Lake Ontario and Lake Superior stay mostly open and can produce all winter.

Lake Erie

80%

average annual maximum ice cover; 34 of 53 winters peaked at 90% or more. The shallowest Great Lake freezes, and its snow machine stops.

Lake Ontario

29%

average annual maximum ice cover; only 7 of 53 winters even reached 50%. The deep lake stays open, and its belt keeps running.

Our averages, computed from NOAA GLERL’s daily Great Lakes ice cover record (GLICD), ice years 1973 to 2025: for each winter we take the season’s peak daily lake-averaged ice cover, then average those peaks.

A dark wall of lake effect snow advancing across Lake Erie toward the Buffalo waterfront
The wall of snow: the leading edge of the November 2014 lake effect band advancing on Buffalo, from the NOAA Photo Library. NWS Buffalo wrote that the band edge was so sharp "many described it as a wall of snow"; every Great Lakes belt town knows a smaller version of this sky. “Snowfall descending on the Buffalo Southtowns” — NOAA Photo Library, NWS Collection — Public domain
Common questions

Syracuse lake effect snow FAQ

City of Buffalo boundary sign at night in wind driven lake effect snow
The city line at night during the November 2014 storm, photographed by Anthony Quintano. Inside a band, rates of 3 to 6 inches per hour with wind are what a Lake Effect Snow Warning is written for. “Historic Lake Effect Snow Hits Buffalo New York Area” by Anthony Quintano, CC BY 2.0