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General Edward Lawrence Logan International Airport turbulence forecast

Boston, United States

Jet-stream + mountain-wave corridor

BOS (Boston, United States) sits at 42.36°N, 71.01°W, 20 ft elevation — coastal with the Appalachians nearby.

Elevation
Sea level
20 ft
Latitude band
Mid latitude
42.4° N
Jet stream
Dominant — frequent CAT exposure
Convective risk
Warm-season

About BOS

Major airport serving Boston, United States.

Climate
Mid-latitude maritime — variable, wind-driven weather
Nearby terrain
Appalachians
Geography
Coastal — marine-influenced airmass

What to expect on departures

Computed from BOS's geography and climate

Boston 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. The Appalachians sit upwind of BOS on prevailing flow days, generating mountain-wave turbulence that can extend several hundred kilometres downwind at cruise level. The lee-wave risk is highest when December–February winds at FL300 cross the Appalachians at near-perpendicular angles. Warm-season convection (June–August) drives the dominant turbulence pattern from BOS — afternoon thunderstorm cells are routed around but their wake turbulence and gust fronts can still affect arrivals and departures. BOS's coastal position means departures often transit from the cool marine boundary layer into warmer continental air within minutes of takeoff — a brief but reliable bumpy transition on warm-season afternoons when the sea breeze is set up.

Climbout notes

Standard Instrument Departures (SIDs) often route around terrain; on strong-wind days, low-level turbulence in the lee of the hills is common in the first few thousand feet.

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. Mountain-wave activity near the Appalachians peaks in the cold season when upper-level winds blow hardest across the range.

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

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BOS turbulence FAQ

Is turbulence common on flights from BOS?

General Edward Lawrence Logan International Airport is best described as a jet-stream + mountain-wave corridor. Boston sits squarely under the mid-latitude jet, north of which most long-haul corridors run.

When is turbulence worst for Boston 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.

Does the terrain around Boston affect turbulence?

Yes — the Appalachians lie close enough to generate mountain-wave turbulence on days with strong upper-level winds. These waves can propagate hundreds of kilometres downwind, so they sometimes affect cruise even after you've left the immediate area.

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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