Abstract:Zusammenfassung --So wie ffir das Himmelsbild in einer einheitlichen Lnft, masse der vertikale Temperaturgradient die wichtigste Rolle splelt, so erweist slch ffir den Wetterablanf beim Kaltfrontdurchgang die vertikale Temperatnrsehichtung im Frontbereich yon entscheidender Bedeutung. In den 1Registrierungen der meteorologischen Elemente zeigt sich meist dentlich der Unterschied zwischen ~ stabilen ~ und ~c labilen ~ Kaltfronten.Summary-As significant the part, played by the vertical lapse rate of temperature … Show more
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