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London Heathrow Airport turbulence forecast

London, United Kingdom

High-latitude airport

LHR (London, United Kingdom) sits at 51.47°N, 0.46°W, 83 ft elevation — inland.

Elevation
Sea level
83 ft
Latitude band
Subpolar
51.5° N
Jet stream
Seasonal — strongest in winter
Convective risk
Low

About LHR

Europe's busiest airport and major global aviation hub.

Climate
Subpolar — long winters, short cool summers

What to expect on departures

Computed from LHR's geography and climate

The jet stream meanders across this latitude seasonally — LHR sees its strongest CAT exposure in December–February, when the polar jet pushes equatorward and routes intersect it more often. June-onwards departures climb into cleaner upper-level flow.

Climbout notes

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

Turbulence conditions

Transatlantic flights are frequently affected by the North Atlantic jet stream. Westbound flights typically encounter more turbulence due to strong headwinds. Winter sees increased CAT activity.

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.

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

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LHR turbulence FAQ

Is turbulence common on flights from LHR?

London Heathrow Airport is best described as a high-latitude airport. The jet stream meanders across this latitude seasonally — LHR sees its strongest CAT exposure in December–February, when the polar jet pushes equatorward and routes intersect it more often.

When is turbulence worst for London 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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