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Amsterdam Schiphol Airport turbulence forecast

Amsterdam, Netherlands

High-latitude airport

AMS (Amsterdam, Netherlands) sits at 52.31°N, 4.76°E, 11 ft below sea level — inland.

Elevation
Sea level
11 ft below sea level
Latitude band
Subpolar
52.3° N
Jet stream
Seasonal — strongest in winter
Convective risk
Low

About AMS

Major European hub known for efficient connections.

Climate
Subpolar — long winters, short cool summers

What to expect on departures

Computed from AMS's geography and climate

The jet stream meanders across this latitude seasonally — AMS 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 Amsterdam occurs at cruise rather than immediately after takeoff.

Turbulence conditions

North Sea weather can be variable. Transatlantic routes cross the jet stream. Generally similar turbulence patterns to other Northern European airports.

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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AMS turbulence FAQ

Is turbulence common on flights from AMS?

Amsterdam Schiphol Airport is best described as a high-latitude airport. The jet stream meanders across this latitude seasonally — AMS 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 Amsterdam 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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