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SUBAsia Pacific

Juanda International Airport turbulence forecast

Surabaya, Indonesia

Tropical convective airport

SUB (Surabaya, Indonesia) sits at 7.38°S, 112.79°E, 9 ft elevation — coastal.

Elevation
Sea level
9 ft
Latitude band
Tropical
7.4° S
Jet stream
Rare — tropical / low-latitude
Convective risk
Year-round

About SUB

Major airport serving Surabaya, Indonesia.

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

What to expect on departures

Computed from SUB'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 SUB. Convective weather closer to the surface is the dominant turbulence source instead. Surabaya's tropical climate means convective build-up is a year-round concern — afternoon and early-evening departures from SUB 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

Departing from SUB?

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SUB turbulence FAQ

Is turbulence common on flights from SUB?

Juanda 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 SUB.

When is turbulence worst for Surabaya 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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