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Route turbulence forecast

Seoul Manila

Turbulence forecast for flights from Incheon International Airport (ICN) to Ninoy Aquino International Airport (MNL).

Standard route profile
Distance
2,609 km
1,409 nm
Typical duration
3h 51m
Ground-speed estimate
Cruise
FL370
37,000 ft
Jet stream
Low — limited jet crossings

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Get a segment-by-segment turbulence forecast for any scheduled flight from ICN to MNL, with live wind and pilot reports.

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What to expect on this route

Southbound · Great-circle bearing -167°

Most of the route sits away from the strongest jet-stream zones, so clear-air turbulence is less common than on long east-west crossings. A large portion of the flight crosses open ocean (North Pacific), where upper-level conditions are generally smoother than over continental terrain.

Ocean / water segments
North Pacific

Seasonal turbulence pattern

This corridor is most turbulent in the northern winter (Nov–Mar), when the jet stream is strongest and sits closer to the route.

Peak turbulence
November–March (Northern Hemisphere winter)
Typically calmest
Late spring to early autumn (May–September)

ICNMNL turbulence FAQ

Is the Seoul to Manila flight usually bumpy?

Most of the 2,609 km route sits in the mixed band with low jet-stream exposure. Historically that means most flights cruise in smooth air, with turbulence limited to short sectors near weather systems.

When is the best time to fly ICN to MNL for a smooth flight?

Statistically, Late spring to early autumn (May–September) sees the calmest conditions for this corridor. Within any season, morning departures see less convective (thunderstorm-driven) turbulence than afternoon flights.

How long is the flight from ICN to MNL?

Block time is usually around 3h 51m direct, cruising at approximately FL370 (37,000 ft). Actual duration varies with winds — tailwinds can shave 15–30 minutes, headwinds can add 30+ minutes on this southbound sector.

How accurate is Turbcast's forecast for this route?

We use live NOAA Aviation Weather Center pilot reports (PIREPs), SIGMETs and AIRMETs, layered with physics-based Ellrod and Richardson-number calculations 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 value.

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