The influence of deep convection on HCHO and HO in the upper troposphere over Europe

The influence of deep convection on HCHO and HO in the upper troposphere over Europe

Deep convection is an efficient mechanism for vertical trace gas transport from Earth's surface to the upper troposphere (UT). The convective redistribution of short-lived trace gases emitted at the surface typically results in a C-shaped profile. This redistribution mechanism can impact ph...

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Bibliographic Details
Main Authors:	H. Bozem, A. Pozzer, H. Harder, M. Martinez, J. Williams, J. Lelieveld, H. Fischer
Format:	Article
Language:	English
Published:	Copernicus Publications 2017-10-01
Series:	Atmospheric Chemistry and Physics
Online Access:	https://www.atmos-chem-phys.net/17/11835/2017/acp-17-11835-2017.pdf

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