Chemtrails at Oslo Gardermoen (OSL)

Oslo, Norway · 60.20°N, 11.08°E · Last updated: Mon, 20 Apr 2026 13:24:12 GMT

Current Contrail Conditions

Moderate Likelihood4/8 levels favorable

4 of 8 atmospheric pressure levels currently show conditions favorable for contrail formation.

Solar visibility: Good · Sun elevation: 35.9°

Atmospheric Conditions by Pressure Level

ChemTracker monitors 8 pressure levels above Oslo Gardermoen. Contrails form when temperature is below the Schmidt-Appleman threshold and relative humidity with respect to ice (RH-ice) exceeds 70%.

PressureAltitudeTemp (°C)RH-water (%)RH-ice (%)Contrail
150 hPa44,327 ft-5235Unlikely
200 hPa38,637 ft-53.51017Unlikely
225 hPa36,216 ft-562644Unlikely
250 hPa34,004 ft-5976132Likely
275 hPa31,965 ft-5891157Likely
300 hPa30,070 ft-5474124Likely
350 hPa26,636 ft-46.36297Likely
400 hPa23,578 ft-38.84261Unlikely

Solar Visibility Over Oslo Gardermoen

Visibility RatingGood
Sun Elevation35.9°
Visibility Factor70%

Solar visibility determines how well contrails can be observed from the ground. Higher sun elevation means better backlit visibility of trail formation above Oslo Gardermoen.

Frequently Asked Questions

Are there chemtrails at Oslo Gardermoen today?

ChemTracker monitors real-time atmospheric conditions above Oslo Gardermoen (OSL) to predict contrail formation. Currently, 4 of 8 pressure levels show conditions favorable for contrail formation — indicating moderate likelihood of persistent trails above this airport.

Why do planes at Oslo Gardermoen leave trails?

Aircraft departing or overflying Oslo Gardermoen (OSL) produce contrails when hot, humid jet exhaust mixes with cold ambient air at cruising altitude. This forms ice crystals that become visible as white trails. Contrails persist when the surrounding air is supersaturated with respect to ice (RH-ice above 100%), which can cause them to spread into cirrus-like haze lasting hours.

How does ChemTracker monitor aircraft at Oslo Gardermoen?

ChemTracker uses live ADS-B transponder data to track every aircraft in the airspace around Oslo Gardermoen (OSL) in real time. Each aircraft's altitude is cross-referenced against atmospheric data from Open-Meteo at 8 pressure levels. The app shows flight numbers, current altitudes, and whether atmospheric conditions at each level are favorable for contrail formation.

What atmospheric conditions cause contrails at Oslo Gardermoen?

Contrails form above Oslo when air temperature drops below approximately −40°C at cruising altitude (typically 8,000–12,000 metres). The Schmidt-Appleman criterion calculates the precise threshold based on ambient pressure, relative humidity, and engine efficiency. When relative humidity with respect to ice exceeds 100%, contrails persist and spread. ChemTracker checks all 8 pressure levels above Oslo Gardermoen for these conditions every 30 minutes.

Nearby Airports & Related Pages

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See every aircraft above Oslo with its altitude, flight number, and whether atmospheric conditions at that pressure level are favorable for trail formation.

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