Lac Saint-Jean freeze shows the lake partly solidified with ice covering its surface during the winter months.
Lac Saint-Jean Freeze lake view
Lake Freeze Profile

When Does Lac Saint-Jean Freeze? Seasonal Ice Cover and Spring Breakup

A regularly frozen Quebec lake with a December freeze-up and a closely watched May ice departure.

Freeze PatternUsually Fully FreezesFreeze-UpAround early to mid-DecemberIce-OffUsually early to mid-May under the local ice-departure criterionFull FreezeRegularLocationQuebec, Canada
Ice Cover TypeComplete Seasonal Ice
Primary DriverCold Continental Winters
Observed TrendA longer open-water season is projected, with earlier spring ice departure and later winter freeze-up
Why It Freezes This Way

Shallow bays and nearshore water freeze first. Sustained subfreezing weather then extends ice across the lake, while wind and waves can break early thin ice and delay establishment of a continuous cover over exposed open water.

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 Lac Saint-Jean?

Quebec · Canada

48.5944° N · 72.0306° W
Loading map…
Lac Saint-JeanQuebec · Canada
World View

Lac Saint-Jean on the Globe

Rotate the world or focus directly on the lake.

Loading world view…
Measurements

Measured Ice and Freeze Data

Historical Open-Water Period, 1958–2023213daysGovernment Environmental AssessmentQuébec Environmental Assessment Registry — Lac Saint-Jean 2028–2037 Impact Study, Volume 2Evidence: Moderate
2024 Open-Water Period246daysTechnical MonitoringQuébec Environmental Assessment Registry — Lac Saint-Jean 2024 Technical Follow-upEvidence: High
2026 Ice-Departure Date, 70% Open-Water CriterionMay 11, 2026Aerial Observation RecordLe Lac-St-Jean — 2026 Ice Departure ObservationEvidence: Moderate
Ice Year

Freeze and Ice Cover Through the Year

JANSeasonal Ice Cover
FEBSeasonal Ice Cover
MARSeasonal Ice Cover
APRSeasonal Ice Cover
MAYTypical Ice Departure
JUNTypical Open-Water Period
JULTypical Open-Water Period
AUGTypical Open-Water Period
SEPTypical Open-Water Period
OCTTypical Open-Water Period
NOVTypical Open-Water Period
DECTypical Freeze-Up Period

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

Evidence

Evidence Behind the Freeze Profile

References

Sources

Lac Saint-Jean normally develops a lake-wide winter ice cover, but the transition from open water to a continuous frozen surface is gradual. Nearshore ice can appear well before exposed parts of the lake lock up, and the spring “ice departure” record uses a defined open-water threshold rather than requiring every remaining piece of ice to disappear.

Why freeze-up does not happen everywhere at once

Lac Saint-Jean covers roughly 1,041 km² and has an average depth of about 11 m, although its deepest areas are much greater. Its broad surface means that early winter conditions can differ substantially between protected shallow water and wind-exposed open water.

Satellite-based analysis found that ice typically begins along the shore and in small, shallow bays. Early ice in these areas can be thin enough to disappear during mild spells. At the same time, wind across unfrozen portions of the lake can maintain waves or break a thin cover that formed during calmer weather. Continuous lake-wide ice therefore represents a later stage of freeze-up, not the first appearance of ice around the shoreline.

December is the key transition from open water to winter cover

Long-term assessments place freeze-up around the first part of December. A recent analysis of the 1958–2023 period produced a characteristic freeze-up date near December 9, while an earlier reference-period assessment placed it near December 10. Observations used in the newer study likewise center the freeze transition in December rather than on a fixed annual date.

This distinction matters because short periods of early shoreline ice do not necessarily mark the end of the open-water season. The lake can still contain large exposed areas after ice has begun forming locally.

What the traditional spring “ice departure” date actually measures

Lac Saint-Jean has an unusually recognizable local spring ice record. Since the late twentieth century, aerial observations have been used to judge the state of the lake. The traditional departure date is reached when approximately 70% of the lake surface is open water.

That definition means the recorded date is not the instant when the final ice disappears. It is a repeatable threshold intended to describe the major transition from the winter cover to predominantly open water. In 2026 that threshold was reached on May 11. The long-term timing is generally centered in early May, but individual springs can depart substantially from that central tendency.

The 2024 season illustrates the size of year-to-year variability

The 2024 technical record stands out because the lake reached its spring ice-departure condition on April 17 and did not reach freeze-up until December 19. That produced a 246-day open-water period. The same technical assessment compared this with a 1991–2024 historical range of roughly 201 to 231 days.

A season such as 2024 should not be treated as the normal calendar for Lac Saint-Jean. It demonstrates instead how both spring breakup and autumn freeze-up can shift enough to change the annual ice season by several weeks.

Projected change is toward a longer open-water season

The latest environmental assessment separates historical observations from modeled future conditions. Its historical 1958–2023 series gives an open-water period of about 213 days, with ice departure near May 10 and freeze-up near December 9.

Under the climate scenarios used in that assessment, the median seasonal boundaries move farther apart. The modeling places ice departure near May 2 and freeze-up near December 17 around the 2040 horizon, followed by approximately April 29 and December 21 around 2070. These dates are scenario-based projections rather than predictions for any individual year, but they describe a consistent physical direction: less of the calendar occupied by the seasonal ice cover and more by open water.

Related Profiles

Similar Lakes by Freeze Pattern