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Wendekreiswüsten – Entstehung

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Wendekreiswüsten – Entstehung

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Trockene Wüsten im Subtropen

Created by

Oliver Emanuel
Oliver Emanuel
Spain

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Wendekreiswüsten – EntstehungOnline version

Trockene Wüsten im Subtropen

by Oliver Emanuel
1

Die Innertropische Konvergenzzone ( ) ist eine Zone äquatornaher Konvergenz und , in der sich die beider Hemisphären kreuzen . Hier steigt durch die - Position der Sonne warme , Luft auf und kühlt sich in der Höhe ab , was fast täglich zu führt .

2

Wendekreiswüsten entstehen vor allem in der Zone rund um Grad nördlicher bzw . südlicher Breite .
Die - Zirkulation führt dort zur trockener Luft ( Antipassat ) . Durch das " Herunter Fallen " der Luft aus höheren Luftschichten wird die Luft am Boden ( Hochdruckgebiet ) .
Wie die Luft in einer erwärmt sich dadurch diese Luft ohne direkte Energiezufuhr ( ) . Durch diese Erwärmung wird die Wolkenbildung gehemmt wird und wenig fällt . Die warme , trockene Luft verhindert Ansammlung von Feuchtigkeit , während Verdunstung hoch bleibt .

 
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