The lake Champlain freeze shows a thick ice cover, indicating cold winter temperatures and the usual timing of ice formation on the lake.
Lake Champlain Freeze lake view
Lake Freeze Profile

How Often Does Lake Champlain Freeze Over?

Protected bays ice readily, while full closure across the broad lake is now intermittent.

Freeze PatternVariable Full/Partial FreezeFreeze-UpAverage freeze date across the lake's widest part: February 12Full FreezeIntermittent; assessed in 2024 at about once every five yearsLocationVermont / New York / Quebec, United States / Canada
Ice Cover TypeIntermittent Full Ice
Primary DriverDeep-water heat storage with wind-driven mixing
Observed TrendComplete freeze-over is less frequent than in the early 1900s
Why It Freezes This Way

Shallow and protected bays can freeze while the deep, broad main lake remains open; stored heat and wind exposure delay or disrupt lake-wide closure.

Ice conditions are not a safety rating.Freeze dates and ice-cover records do not determine whether lake ice is safe for walking, skating, vehicles, or other activity.
Interactive Lake Map

Where Is Lake Champlain?

Vermont / New York / Quebec · United States / Canada

44.5000° N · 73.3333° W
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Lake ChamplainVermont / New York / Quebec · United States / Canada
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World View

Lake Champlain on the Globe

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Measurements

Measured Ice and Freeze Data

2026 Official Lake Closure DateFebruary 13, 2026Official MonitoringNational Weather Service Burlington — Dates of Lake Champlain ClosingEvidence: High
Previous NWS-Listed ClosureMarch 8, 2019Official MonitoringNational Weather Service Burlington — Dates of Lake Champlain ClosingEvidence: High
Average Freeze Date Across the Widest PartFebruary 12Government Lake DataLake Champlain Basin Program — Lake and Basin FactsEvidence: Moderate
2024 Assessed Full-Freeze FrequencyAbout 1 in 5yearsGovernment Lake DataLake Champlain Basin Program — 2024 State of the Lake and Ecosystem Indicators ReportEvidence: High
Historical Earliest Recorded ClosureJanuary 7, 1868Historical Monitoring RecordNational Weather Service Burlington — Dates of Lake Champlain ClosingEvidence: Limited
Historical Latest Recorded ClosureMarch 26, 1894Historical Monitoring RecordNational Weather Service Burlington — Dates of Lake Champlain ClosingEvidence: Limited
Ice Year

Freeze and Ice Cover Through the Year

JANDeveloping Winter Ice
FEBMain-Lake Freeze-Over Window When Closure Occurs
MARLate Ice Season and Breakup Transition
APRLate Ice Season and Breakup Transition
MAYTypical Open-Water Period
JUNTypical Open-Water Period
JULTypical Open-Water Period
AUGTypical Open-Water Period
SEPTypical Open-Water Period
OCTTypical Open-Water Period
NOVTypical Open-Water Period
DECDeveloping Winter Ice

Month-level states are shown only when supported. Unclassified months remain explicitly marked.

Evidence

Evidence Behind the Freeze Profile

References

Sources

Lake Champlain develops winter ice regularly, especially in sheltered bays, but the broad lake does not close every year. The National Weather Service listed a full closure on February 13, 2026, the first since March 8, 2019, after six consecutive winters without a listed closure.

What “closed” means on Lake Champlain

Lake Champlain has one of the longer lake-closure records in North America, but the meaning of “closed” has changed with the observing method. Nineteenth-century entries could reflect the end of commercial shipping or visual reports of ice across the broad lake between the Burlington area and the New York shore. Those records cannot always establish that every part of the lake was covered.

Modern monitoring is different. Since 2009, National Weather Service Burlington has archived polar-orbiting satellite imagery to judge approximate ice coverage. Even a modern “iced over” determination can include very small open-water gaps that are not resolved clearly in the imagery. For Lake Champlain, closure is therefore a defined monitoring observation rather than a guarantee of perfectly continuous ice over every square meter of water.

Why the broad lake freezes later than sheltered bays

Lake Champlain is large enough for its basins to respond differently to the same winter. It covers about 455 square miles (1,179 square kilometers), reaches roughly 400 feet (122 meters) at its deepest point, and is divided into distinct sectors that include the Main Lake, South Lake, Malletts Bay, the Northeast Arm and Missisquoi Bay.

The deep Main Lake can retain heat longer than shallow or protected water, while its long open-water reaches remain exposed to wind and wave mixing. Sheltered bays can lose heat and form ice while open portions of the broad lake are still moving. New York State fisheries guidance also notes that Lake Champlain may or may not freeze completely in winter and that strong winds can break established ice apart or pull sections away from one another, creating open water again.

The 2026 freeze in a much longer record

The February 2026 closure was unusual in the recent sequence, but it fits within a record that still contains occasional cold winters capable of closing the broad lake. The 2024 State of the Lake report states that Lake Champlain froze over nearly every year in the early 1900s, whereas complete freeze-over in the recent climate had fallen to about once every five years.

The same report cites modeling that suggests complete freeze-over could decline to roughly once per decade by 2050. A single winter such as 2025–26 does not establish a change in that multi-decadal pattern; it shows that full closure remains possible when cold weather persists long enough for the broad lake to lose its stored heat.

Why the oldest closure dates need context

The historical series includes an earliest listed closure in January and a latest listed closure in late March, but those endpoints come from an era when observing methods were not the same as today. The National Weather Service explicitly treats the older list as informational because source quality and the meaning of “closure” vary through time.

That distinction matters when comparing centuries. The modern satellite-era record is better suited to judging broad-lake ice coverage, while nineteenth-century dates are most useful as evidence that winter closure was documented far more often than it is now. Treating every historical date as if it were produced by the same measurement method would give a false sense of precision.

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