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Noi Bai International Airport turbulence forecast

Hanoi, Vietnam

Tropical convective airport

HAN (Hanoi, Vietnam) sits at 21.22°N, 105.81°E, 39 ft elevation — coastal.

Elevation
Sea level
39 ft
Latitude band
Tropical
21.2° N
Jet stream
Rare — tropical / low-latitude
Convective risk
Year-round

About HAN

Major airport serving Hanoi, Vietnam.

Climate
Tropical coastal — warm, humid, convective
Geography
Coastal — marine-influenced airmass

What to expect on departures

Computed from HAN's geography and climate

At tropical latitude the jet stream is rarely directly overhead, so clear-air turbulence is less of a routine concern from HAN. Convective weather closer to the surface is the dominant turbulence source instead. Hanoi's tropical climate means convective build-up is a year-round concern — afternoon and early-evening departures from HAN encounter the most cell activity. Morning slots and red-eye departures are typically the smoothest of the day.

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

Convective turbulence cycles with the local wet/dry season rather than a strict calendar month — check regional rainy-season dates for the most accurate risk window.

Peak turbulence
Regional wet season
Typically calmest
Regional dry season

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HAN turbulence FAQ

Is turbulence common on flights from HAN?

Noi Bai International Airport is best described as a tropical convective airport. At tropical latitude the jet stream is rarely directly overhead, so clear-air turbulence is less of a routine concern from HAN.

When is turbulence worst for Hanoi flights?

Convective turbulence cycles with the local wet/dry season rather than a strict calendar month — check regional rainy-season dates for the most accurate risk window. Peak turbulence window: Regional wet season. Typically calmest: Regional dry season.

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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