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McCarran International Airport turbulence forecast

Las Vegas, United States

Jet-stream + mountain-wave corridor

LAS (Las Vegas, United States) sits at 36.08°N, 115.15°W, 2,181 ft elevation — coastal with the Rocky Mountains and Sierra Nevada nearby.

Elevation
Moderate (2–5,000 ft)
2,181 ft
Latitude band
Mid latitude
36.1° N
Jet stream
Dominant — frequent CAT exposure
Convective risk
Warm-season

About LAS

Major airport serving Las Vegas, United States.

Climate
Mid-latitude maritime — variable, wind-driven weather
Nearby terrain
Rocky Mountains · Sierra Nevada
Geography
Coastal — marine-influenced airmass

What to expect on departures

Computed from LAS's geography and climate

The 2,181 ft elevation puts LAS above most of the densest surface air, so initial climb is brisk but the airport itself sits inside any low-level turbulence patterns. Las Vegas sits squarely under the mid-latitude jet, north of which most long-haul corridors run. Clear-air turbulence (CAT) at cruise is the most common source of bumps on departures from here, especially during December–February when the jet is at its strongest. The Rocky Mountains and Sierra Nevada sit upwind of LAS on prevailing flow days, generating mountain-wave turbulence that can extend several hundred kilometres downwind at cruise level. The lee-wave risk is highest when December–February winds at FL300 cross the Rocky Mountains at near-perpendicular angles. Warm-season convection (June–August) drives the dominant turbulence pattern from LAS — afternoon thunderstorm cells are routed around but their wake turbulence and gust fronts can still affect arrivals and departures. LAS'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

Standard Instrument Departures (SIDs) often route around terrain; on strong-wind days, low-level turbulence in the lee of the hills is common in the first few thousand feet.

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. Summer (June–August) is peak thunderstorm season — convective turbulence is the dominant warm-season risk. Mountain-wave activity near the Rocky Mountains peaks in the cold season when upper-level winds blow hardest across the range.

Peak turbulence
November–February (strong jet)
Typically calmest
May–September

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LAS turbulence FAQ

Is turbulence common on flights from LAS?

McCarran International Airport is best described as a jet-stream + mountain-wave corridor. The 2,181 ft elevation puts LAS above most of the densest surface air, so initial climb is brisk but the airport itself sits inside any low-level turbulence patterns.

When is turbulence worst for Las Vegas 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.

Does the terrain around Las Vegas affect turbulence?

Yes — the Rocky Mountains and Sierra Nevada lie close enough to generate mountain-wave turbulence on days with strong upper-level winds. These waves can propagate hundreds of kilometres downwind, so they sometimes affect cruise even after you've left the immediate area.

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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