Wenn heiße, feuchte Abgase aus Flugzeugtriebwerken in großer Höhe auf kalte Luft treffen, der darin enthaltene Wasserdampf kondensiert und zu Eiskristallen gefriert, entstehen am Himmel Kondensstreifen. Bleiben sie über längere Zeit bestehen und breiten sich aus, können sie nach und nach zur Bildung von Zirruswolken führen, die Wärme in der Atmosphäre halten und so einen wärmenden Klimaeffekt erzeugen.
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