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1. Global chemistry-climate modelling with EMAC


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2. Global chemistry-climate modelling with EMAC


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3. Nonlinearity in regression analyses of atmospheric ozone


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4. Einfluß des Ozeans auf die Stratosphäre


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5. Höhere tropische Meeresoberflächentemperaturen verstärken das tropische Aufsteigen mittels hochreichender Konvektion


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6. Der Klimawandel und die Erholung der Ozonschicht


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7. Detection of surface heterogeneity in eddy covariance data


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8. Der Klimawandel und die Erholung der Ozonschicht


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9. Höhere tropische Meeresoberflächentemperaturen verstärken das tropische Aufsteigen mittels hochreichender Konvektion


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10. Einfluß des Ozeans auf die Stratosphäre


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