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Dublin Airport turbulence forecast

Dublin, Ireland

High-latitude airport

DUB (Dublin, Ireland) sits at 53.42°N, 6.27°W, 242 ft elevation — coastal.

Elevation
Sea level
242 ft
Latitude band
Subpolar
53.4° N
Jet stream
Seasonal — strongest in winter
Convective risk
Low

About DUB

Major airport serving Dublin, Ireland.

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

What to expect on departures

Computed from DUB's geography and climate

The jet stream meanders across this latitude seasonally — DUB 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. DUB'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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DUB turbulence FAQ

Is turbulence common on flights from DUB?

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