Hans-Jurg Jost

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[1] We use in situ measurements of water vapor (H 2 O), ozone (O 3), carbon dioxide (CO 2), carbon monoxide (CO), nitric oxide (NO), and total reactive nitrogen (NO y) obtained during the CRYSTAL-FACE campaign in July 2002 to study summertime transport in the subtropical lowermost stratosphere. We use an objective methodology to distinguish the latitudinal(More)