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Snow Day Predictor Canada

Vancouver · British Columbia · 2026–27 season

Snow Day Predictor VancouverWill school be cancelled tomorrow in Vancouver?

Live overnight forecast for the City of Vancouver, the North Shore, Burnaby, Richmond, and the wider Lower Mainland. The predictor tunes to Vancouver SD #39, North Vancouver SD #44, West Vancouver SD #45, and Conseil scolaire francophone (CSF) closure patterns, with bus cancellation probability returned separately for each district.

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Multi-model forecast, five-factor closure engine, province-aware results. No sign-up, no tracking of your queries.

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What makes Vancouver unique

Vancouver closes schools for less snow than any major Canadian city, often around 5 to 10 cm. The combination of coastal infrastructure unprepared for sustained snow, the Pacific atmospheric river pattern, and Arctic outflow events through the Fraser Valley creates a winter pattern unlike any other Canadian city.

Lower Mainland forecast

Vancouver snow day forecast, what to expect this winter

Vancouver sits on the Strait of Georgia at the western edge of the Coast Mountains, a setting that produces one of the most unusual winter climates in Canada. The city averages only around 35 to 40 cm of snow per year at sea level, less than a tenth of what Quebec City sees, yet Vancouver schools close at snow accumulations that would not raise an eyebrow in Calgary or Winnipeg. The reason is structural: the City of Vancouver, the District of North Vancouver, and surrounding municipalities maintain a fraction of the plow and salt fleet of comparably sized prairie cities, because they would sit idle in a normal Lower Mainland winter. When snow does fall and sticks, the road network is overwhelmed within hours.

School operations in Vancouver are fragmented across multiple independent districts. Vancouver School District #39 serves the City of Vancouver proper, from Kitsilano and Point Grey across the West Side through Mount Pleasant, the East Side, and the River District. North Vancouver SD #44 and West Vancouver SD #45 cover the North Shore, where elevation alone can mean 30 cm of snow at British Properties while False Creek sees only rain. The Conseil scolaire francophone de la Colombie-Britannique (SD #93) operates French-language schools province-wide, including several in Vancouver, and makes closure decisions independently. Each district director calls the morning before 6:00 am, and on a typical North Shore snow event West Van will close while Vancouver SD #39 holds open.

For Lower Mainland families, the practical question is rarely "how much snow will fall" but rather "does the snow stick, and does it stick at my elevation." A Pineapple Express atmospheric river can drop 80 mm of rain on Kitsilano while burying Cypress Bowl in a metre of snow, and the school decision depends almost entirely on the freezing level. Our forecast pulls hourly data at your exact coordinates rather than averaging across the Lower Mainland, which is essential in a city where the difference between school open and school closed can be 200 metres of elevation.

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School boards

Vancouver school boards we model

The boards and transportation operators that make the morning closure call for Vancouver.

  • Vancouver School District #39 (VSB)

    The public school district for the City of Vancouver, serving over 47,000 students from Kitsilano and Point Grey through Mount Pleasant, the East Side, and the River District. Makes its own closure call before 6:00 am.

  • North Vancouver SD #44 and West Vancouver SD #45

    Adjacent North Shore districts covering Lynn Valley, Deep Cove, Edgemont, Ambleside, and the British Properties. Often close in concert when North Shore elevation snow exceeds City of Vancouver accumulation, which is common during Arctic outflow events.

  • Conseil scolaire francophone de la Colombie-Britannique (SD #93)

    The French-language public school authority for all of British Columbia, with schools in Vancouver including École Rose-des-Vents and École Anne-Hébert. Closure decisions are made centrally and may not align with Vancouver SD #39.

  • Independent and Catholic schools (CISVA)

    The Catholic Independent Schools of the Vancouver Archdiocese (CISVA) and other independent schools such as St. George’s, Crofton House, and York House operate outside the public boards and make their own weather calls, though most align loosely with the surrounding public district.

Bus transportation

Vancouver SD #39 contracts its own bus operators where buses are used, though most students walk or use TransLink transit rather than a yellow bus. There is no inter-district consortium in the Lower Mainland, so North Vancouver SD #44, West Vancouver SD #45, and Vancouver SD #39 each make independent transportation calls. Each school district makes its own decision by 6:00 am the morning of, posted to the district website and notified through SchoolMessenger. TransLink bus and SkyTrain service runs in nearly all winter weather, which is why VSB rarely closes for a storm that would shut down a bus-dependent suburban district.

Local weather

Vancouver’s signature winter weather patterns

The phenomena that produce most Vancouver snow days.

  • Pacific atmospheric river (Pineapple Express)

    A narrow corridor of moist subtropical air streaming northeast from near Hawaii, delivering 50 to 150 mm of rain at sea level and one to two metres of snow at elevation in 24 to 48 hours. The freezing level decides the school outcome: a high freezing level means rain on the city and a closure of Sea to Sky Highway only, while a dropping freezing level mid-event can turn rain to heavy wet snow across Vancouver in a few hours.

  • Arctic outflow through the Fraser Valley

    Cold continental air drains out of the BC Interior through the Fraser Valley, accelerating into the Lower Mainland as a sustained easterly wind. Temperatures can drop from 8 °C to −10 °C in a single day, with wind chills near −20 °C in Richmond and South Vancouver. Arctic outflow is the trigger for nearly every multi-day cold snap and most Vancouver snow events that actually accumulate.

  • Sea-level cold-air pooling

    Under clear, calm conditions following an Arctic outflow, the coldest air settles in low-lying neighbourhoods such as the River District, Marpole, and parts of Richmond. These areas can run 3 to 5 °C colder than Kitsilano or the West End in the same overnight period, which is enough to flip a rain forecast to snow on the south side of the city while the West Side stays clear.

  • North Shore mountain snow

    Cypress, Grouse, and Mount Seymour can hold metres of snowpack while the City of Vancouver shows bare pavement. Schools in the British Properties, upper Lynn Valley, and Edgemont sit at 200 to 400 metres of elevation, well above the typical freezing level during a coastal storm, which is why West Vancouver SD #45 and North Vancouver SD #44 close on days that Vancouver SD #39 does not.

  • Freezing rain at the elevation transition zone

    When warm air aloft overruns a shallow cold layer near the surface, freezing rain forms in a narrow elevation band, often between 100 and 300 metres on the North Shore and along the Burnaby Heights ridge. The band can sit directly over schools in upper Capilano or SFU-area Burnaby while leaving downtown Vancouver in plain rain.

History

Notable Vancouver snow days in recent winters

Storms and ice events that shaped how Vancouver school boards approach the morning call.

  • Lower Mainland snowstorm

    December 17-20, 2008

    A multi-day Arctic outflow event delivered more than 30 cm of snow to the City of Vancouver, with deeper accumulations on the North Shore and in the Fraser Valley. Vancouver SD #39 closed schools, an unusual full-district closure. TransLink service was reduced and Vancouver International Airport saw extended delays. The event remains a benchmark Lower Mainland snowstorm and is regularly cited in district closure debriefs.

  • Overnight snow event across Vancouver and Surrey

    January 6-7, 2020

    Around 30 cm of snow fell overnight from a coastal low that tracked unusually far south, hitting Surrey, Delta, Richmond, and the south side of Vancouver hardest. Surrey schools closed; Vancouver SD #39 cancelled buses and ran a partial day. The event illustrated how a single storm can cross the Lower Mainland with very different local accumulations.

  • Early-season Lower Mainland snow

    November 14, 2022

    An early-season Arctic outflow combined with coastal moisture to drop 10 to 20 cm of snow across the Lower Mainland on a Monday morning. Vancouver SD #39 cancelled bus routes and a number of independent schools closed outright. The November timing caught the city before winter road treatment crews were fully deployed.

  • Coastal BC Arctic outflow event

    December 18-23, 2022

    A prolonged Arctic outflow over the final school week before Christmas brought sustained sub-zero temperatures, blowing snow, and freezing rain to the Lower Mainland. North Vancouver SD #44 and West Vancouver SD #45 closed for multiple days; Vancouver SD #39 ran modified schedules. The event coincided with widespread BC Ferries cancellations.

  • Atmospheric river and Sumas flooding aftermath

    November 2021

    A series of atmospheric rivers in mid-November 2021 produced catastrophic flooding in Abbotsford and the Sumas Prairie, washed out the Coquihalla Highway, and isolated parts of the Fraser Valley. While the City of Vancouver itself saw rain rather than snow, schools in surrounding districts closed and Vancouver SD #39 operations were affected by supply chain and staffing disruptions. The event reshaped how the province discusses winter weather risk in the Lower Mainland.

  • February 2019 snow event

    February 12, 2019

    A coastal storm with a low freezing level dropped 15 to 25 cm of snow across the City of Vancouver and the North Shore. Vancouver SD #39 closed schools, North Vancouver SD #44 and West Vancouver SD #45 closed for two days, and TransLink trolley bus service was suspended on multiple routes. A textbook example of a "stuck below freezing" Lower Mainland event.

FAQ

Vancouver snow day frequently asked questions

The 7 questions Vancouver parents and teachers ask us most.

Will Vancouver SD #39 close tomorrow?

Type your Vancouver postal code or "Vancouver, British Columbia" into the predictor above. Vancouver School District #39 makes its own closure call by 6:00 am the morning of, posted to the VSB website and notified through SchoolMessenger. VSB closures are rare but happen at lower snow thresholds than almost any other major Canadian city, typically around 5 to 10 cm of accumulated snow on the ground combined with continuing precipitation. The predictor returns both a school-closure probability and a separate bus-cancellation probability for the night before.

Why does Vancouver close for less snow than Calgary or Edmonton?

Vancouver averages only 35 to 40 cm of snow a year at sea level, so the City of Vancouver and surrounding municipalities maintain only a fraction of the plow, salt, and brine capacity of prairie cities. A 10 cm snowfall in Calgary clears in hours; the same snowfall in Vancouver can sit on residential streets for days, with freeze-thaw cycles turning it to ice. School bus routes, sidewalks, and crosswalks become unsafe long before they would in Edmonton or Winnipeg, which is why Vancouver SD #39 and the North Shore districts have lower closure thresholds.

What is the Pineapple Express and how does it affect Vancouver schools?

The Pineapple Express is the popular name for a Pacific atmospheric river, a narrow corridor of warm, very moist air streaming northeast from near Hawaii into coastal British Columbia. For Vancouver schools, the key variable is the freezing level. A high-freezing-level Pineapple Express brings heavy rain to the city with metres of snow only at Cypress, Grouse, and Whistler, and schools stay open. A dropping freezing level mid-event can flip Vancouver to heavy wet snow within hours and trigger closures across Vancouver SD #39 and the North Shore districts.

Will school be cancelled on the North Shore (West Van, North Van) tomorrow?

The North Shore is served by two separate districts: North Vancouver SD #44 covers Lynn Valley, Deep Cove, and central North Van, and West Vancouver SD #45 covers Ambleside, the British Properties, Caulfeild, and Lions Bay. Both districts close more readily than Vancouver SD #39 because their catchments include schools at 200 to 400 metres of elevation, where snow accumulates while downtown Vancouver sees rain. On a typical North Shore snow event, expect SD #44 and SD #45 to make the same call within an hour of each other, often closing while VSB stays open.

How does an atmospheric river differ from a normal snowstorm for Vancouver?

A normal snowstorm in most Canadian cities involves cold air, a low-pressure system, and a relatively predictable snow ratio. A Pacific atmospheric river is fundamentally a rain event with a snow component that depends on the freezing level. Total precipitation can exceed 100 mm in 24 hours, but only the fraction that falls below freezing accumulates as snow, and that fraction changes hour by hour. For Vancouver school decisions, the question is less "how much snow" and more "what elevation is freezing tonight at 4 am," which is why the predictor pulls freezing-level data alongside surface forecasts.

Do the French CSF schools close with Vancouver SD #39?

Not necessarily. The Conseil scolaire francophone de la Colombie-Britannique (CSF, SD #93) operates French-language schools province-wide and makes closure decisions centrally rather than mirroring whatever public district sits over a given school. CSF schools in Vancouver such as École Rose-des-Vents may close on a day when Vancouver SD #39 stays open, or vice versa. Families with children in CSF should check the SD #93 website directly rather than relying on the VSB call.

Will school be cancelled in Kitsilano or Mount Pleasant tomorrow?

Kitsilano and the West Side, along with Mount Pleasant and the central East Side, are all served by Vancouver School District #39, so any closure call applies citywide rather than by neighbourhood. That said, accumulation in Kitsilano, Point Grey, and the West End is often noticeably less than in the River District, Marpole, or the East Side, because sea-level cold-air pooling and slight elevation differences favour the south and east of the city for snow. Enter your specific postal code in the predictor to get the forecast at your exact coordinates; we do not average across the city.

Near Vancouver

Nearby British Columbia cities

Other British Columbia cities our forecast covers — same regional profile, different local weather.

Looking for forecasts across the rest of British Columbia? View the British Columbia hub with all school boards, transportation consortia, weather zones, and a full city directory. Or browse the provinces & territories hub for every Canadian region.

Also in British Columbia: Victoria · Kelowna · Kamloops · Prince George · Nanaimo

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