A visible contrail appears when the water vapor from an aircraft's propulsion condenses into ice crystals within a layer of cold, humid air. Its appearance and persistence depend mainly on temperature, the air's absolute humidity, atmospheric pressure and engine speed, along with the atmospheric turbulence that can dissipate it.
How contrails form
Engine fuel produces water vapor, carbon dioxide and carbon particles. When this vapor comes into contact with very low-temperature air (generally below 0 °C) and with sufficient humidity, it condenses, forming tiny droplets or ice crystals. These particles gather in a thin layer around the fuselage, creating the appearance of a contrail.
Factors that influence visibility and persistence
- Air temperature: The colder the temperature at flight altitude, the greater the likelihood that the vapor will freeze into ice. At altitudes above 8,000 m, the temperature is usually low enough for contrails to form.
- Absolute humidity: This is the actual amount of water vapor present in the air. If humidity is high (above 70% at that altitude level), the exhaust vapor condenses easily; if it is low, the vapor evaporates without leaving a trail.
- Atmospheric pressure: Lower pressure at high altitudes favors evaporation and can cause contrails to fade quickly. Moderate pressure helps the ice crystals remain together.
- Engine speed and exhaust flow: A more powerful engine produces more water vapor and a faster exhaust stream, which increases the likelihood of condensation. Commercial passenger aircraft tend to operate within this higher range.
- Turbulence and wind: If the surrounding air is turbulent, the ice particles scatter and the contrail dissipates within minutes. Under calm wind conditions, the contrail can remain visible for hours.
- Fuel type and exhaust composition: Fuels with a higher water content and lower hydrocarbon content can increase the amount of vapor produced.
- Age and condition of the aircraft: Aircraft with older or more worn engines may release more water vapor.
In short, the presence and duration of a contrail depend on a delicate balance between exhaust vapor, atmospheric conditions and flight dynamics. When conditions are right, the contrail forms and can persist; when they are not, the vapor dissipates without leaving a visible trace.


¡Me fascina la ciencia detrás de las estelas! Ahora entiendo perfectamente por qué algunas desaparecen rápido y otras se quedan en el cielo.
Qué artículo tan completo y bien explicado. Es genial aprender cómo la temperatura y la humedad marcan la diferencia en algo que vemos a diario.