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Shannon Airport turbulence forecast

Shannon, Ireland

High-latitude airport

SNN (Shannon, Ireland) sits at 52.70°N, 8.92°W, 46 ft elevation — coastal.

Elevation
Sea level
46 ft
Latitude band
Subpolar
52.7° N
Jet stream
Seasonal — strongest in winter
Convective risk
Low

About SNN

Major airport serving Shannon, Ireland.

Climate
Subpolar — long winters, short cool summers
Geography
Coastal — marine-influenced airmass

What to expect on departures

Computed from SNN's geography and climate

The jet stream meanders across this latitude seasonally — SNN 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. SNN'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

Climbout typically transitions from cool marine air to warmer continental air — a brief bumpy layer near the boundary is normal on summer afternoons.

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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SNN turbulence FAQ

Is turbulence common on flights from SNN?

Shannon Airport is best described as a high-latitude airport. The jet stream meanders across this latitude seasonally — SNN 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 Shannon 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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