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Live forecasts update automatically; written guidance last reviewed 16 June 2026 by the Canada Edition Weather Desk. Data from Environment and Climate Change Canada and other national met services via Open-Meteo.
Live data from Open-Meteo · updates automatically ·
Check the live forecast above for today’s high and low in Smithers; a classic Bulkley Valley pattern of morning cloud breaking to afternoon sun is expected, with temperatures near seasonal norms.
What’s driving Smithers weather today?
Smithers sits in the Bulkley Valley, tucked between the Coast Mountains and the Babine Range. That geography funnels Pacific moisture, so you’ll often see cloud build-up through the morning before clearing by mid-afternoon. The live forecast above reflects that typical rhythm. For comparison, terrace weather tends to be wetter due to its lower elevation, while burns lake weather sits drier on the Nechako Plateau. Smithers sits right in the transition zone.
What does the extended outlook show?
The smithers weather 14 day outlook suggests a weak ridge building later this week, lifting the cloud and keeping highs near the mid‑teens. If you’re after a longer look, the smithers weather 30 day forecast hints at a cooler end to September. For hour‑by‑hour detail, the smithers weather hourly break down is useful for planning hikes or drives to nearby towns like Terrace and Burns Lake.
Is snow expected soon in Smithers?
Not in the immediate outlook. The live forecast shows overnight lows staying above freezing for the next few days. Typically, the first measurable snow arrives in late October. You can track changes via smithers weather environment canada bulletins.
How does Smithers compare to Terrace or Burns Lake?
Terrace gets about 50% more annual precipitation because Pacific air hits the Coast Mountains first. Burns Lake, east of here, sees colder winter lows and less snowfall. Smithers splits the difference, with moderate rain and snow. For news on local conditions, check smithers news updates.
Why does Smithers get afternoon clearing?
Valley cloud forms overnight as cool air settles. By late morning, sunshine warms the valley floor, breaking the inversion. This “diurnal cycle” is classic in interior BC basins. It’s less pronounced in coastal Terrace, where marine layer lingers.