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St Louis Lambert International Airport turbulence forecast

St. Louis, United States

Mid-latitude jet-exposed hub

STL (St. Louis, United States) sits at 38.75°N, 90.37°W, 618 ft elevation — inland.

Elevation
Low (<2,000 ft)
618 ft
Latitude band
Mid latitude
38.7° N
Jet stream
Dominant — frequent CAT exposure
Convective risk
Warm-season

About STL

Major airport serving St. Louis, United States.

Climate
Mid-latitude continental — strong seasonal cycle

What to expect on departures

Computed from STL's geography and climate

St. Louis sits squarely under the mid-latitude jet, north of which most long-haul corridors run. Clear-air turbulence (CAT) at cruise is the most common source of bumps on departures from here, especially during December–February when the jet is at its strongest. Warm-season convection (June–August) drives the dominant turbulence pattern from STL — afternoon thunderstorm cells are routed around but their wake turbulence and gust fronts can still affect arrivals and departures.

Climbout notes

Climbout is usually unremarkable — most turbulence on flights from St. Louis occurs at cruise rather than immediately after takeoff.

Seasonal pattern

Winter (December–February) brings the strongest jet-stream activity — that's when long-haul departures most often log clear-air turbulence at cruise. Summer (June–August) is peak thunderstorm season — convective turbulence is the dominant warm-season risk.

Peak turbulence
November–February (strong jet)
Typically calmest
May–September

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STL turbulence FAQ

Is turbulence common on flights from STL?

St Louis Lambert International Airport is best described as a mid-latitude jet-exposed hub. St.

When is turbulence worst for St. Louis flights?

Winter (December–February) brings the strongest jet-stream activity — that's when long-haul departures most often log clear-air turbulence at cruise. Peak turbulence window: November–February (strong jet). Typically calmest: May–September.

How accurate are Turbcast forecasts?

We combine live NOAA Aviation Weather Center data (PIREPs, SIGMETs, AIRMETs) with physics-based Ellrod and Richardson-number calculations derived from Open-Meteo pressure-level wind and temperature data. If a source is unavailable for a waypoint we show an em dash rather than invent a number.

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