Nebenstehend wird die Luftblasenbildung in einem animierten AirMeteogramm gezeigt.
Wenn immer mehr Luft erwärmt wird und nachströmt, entsteht eine Art " Luftblase ", welche die ganze Trophosphäre (untere Schicht der Atmosphäre) nach oben ausdehnen kann.
www.meteoblue.comThe rise of air temperature and warming of higher atmosphere layers during the day is shown in an animated AirMeteogramm to the right.
If more and more air warms up and rises, a kind of " air bubble " develops, which can expand the whole trophosphere (lower layer of the atmosphere) upwards.
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