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Ein Rechenmodell zur Beschreibung des Stratosphrischen Ozonkreislaufs

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Brand
Springer Nature
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N/A
Part Number
0
GTIN
9783540064947
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New
Product Description

Das atmosphrische Ozon ist heute Objekt routinemiger meteorologischer Untersuchungen sowie globaler atmosphrischer Forschungsprogramme in experimenteller und theoretischer Hinsicht. Eine Vielzahl geophysikalischer Phnomene lt sich auf die besonderen chemischen und physikalischen Eigen schafte.n des Ozons zurckfhren (Airglow, Photochemie der D-Schicht, Strahlungsbilanz der Mesosphre und Stratosphre, Photochemie langlebiger Spurengase, Photochemie der Stratosphre). Zu den wichtigsten physikalischen Eigenschaften des Ozons zhlt seine Fhigkeit, Strahlungsenergie gewisser Wellenlngenbereiche zu absorbieren. Whrend der gewhnliche Sauerstoff (0 ) fr alle Wellen 2 lngen}..=: 2400 transparent ist, absorbiert Ozon (0 ) in drei meteorologisch wichtigen Bereichen. 3 Im Gebiet zwischen ca. 2000 - 3300 mit einem Maximum bei 2500 findet extrem starke UV -Ab sorption statt. Trotz der uerst geringen atmosphrischen Gesamtozonmengen mit optischen Weglngen zwischen 0, 2 und 0, 4 cm +) verhindert diese Absorptionsfhigkeit ein Eindringen der harten UV -Strah lung (Wellenlngen X 5 3000 ') bis zur Erdoberflche und ist damit von grundlegender Bedeutung fr die Existenz von Leben auf der Erde. Darberhinaus bewirkt die UV -Absorption die Ausbildung des Tempera turmaximums in 50 km Hhe.

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