The dual role of Asian deep convection in cross-tropopause transport of water: hydration and dehydration

Sergey Khaykin1, Martina Kraemer2, Elisabeth J Moyer3, Alexey Lykov4, Silvia Bucci5, Armin Afchine2, Stephan Borrmann6, Francesco Cairo7, Benjamin Clouser3, Francesco D’Amato8, Bernad Legras9, Velentin Mitev10, Renaud Matthey11, Fabrizio Ravegnani7, Christian Rolf12, Alexey Ulanovsky13, Silvia Viciani8, C Michael Volk14, Vladimir A Yushkov13, Fred Stroh15 and StratoClim aircraft campaign team, (1)LATMOS/IPSL, UVSQ, Sorbonne Université, CNRS, Paris Cedex 05, France, (2)Forschungszentrum Juelich, Juelich, Germany, (3)University of Chicago, Geophysical Sciences, Chicago, IL, United States, (4)Central Aerological Observatory of RosHydroMet, Dolgoprudny, Russia, (5)Laboratoire de Météorologie Dynamique ENS, Paris, France, (6)Johannes Gutenberg University, Max Planck Institute for Chemistry, Particle Chemistry, Mainz, Germany, (7)Institute of Atmospheric Science and Climate, ISAC-CNR, Rome, Italy, (8)CNR-INO National Institute of Optics, Florence, Italy, (9)Laboratoire de Météorologie Dynamique Palaiseau, Palaiseau Cedex, France, (10)Centre Suisse d’Electronique et de Microtechnique Neuchatel, Neuchatel, Switzerland, (11)LTF-University of Neuchatel, Neuchatel, Switzerland, (12)Forschungszentrum Juelich, IEK-7, Juelich, Germany, (13)Central Aerological Observatory of RosHydroMet, Moscow, Russia, (14)Institute for Atmospheric and Environmental Research, University of Wuppertal, Wuppertal, Germany, (15)Forschungszentrum Juelich, Jülich, Germany