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Uptake of reactive nitrogen on cirrus cloud particles during INCA
Author(s) -
Ziereis H.,
Minikin A.,
Schlager H.,
Gayet J. F.,
Auriol F.,
Stock P.,
Baehr J.,
Petzold A.,
Schumann U.,
Weinheimer A.,
Ridley B.,
Ström J.
Publication year - 2004
Publication title -
geophysical research letters
Language(s) - English
Resource type - Journals
SCImago Journal Rank - 2.007
H-Index - 273
eISSN - 1944-8007
pISSN - 0094-8276
DOI - 10.1029/2003gl018794
Subject(s) - cirrus , troposphere , ice cloud , ice crystals , atmospheric sciences , aerosol , particulates , middle latitudes , particle (ecology) , environmental science , gas phase , meteorology , chemistry , geology , radiative transfer , physics , oceanography , optics , organic chemistry
The uptake of reactive nitrogen species on ice crystals in cirrus clouds was investigated by simultaneous aircraft‐based measurements of gas‐ and condensed‐phase NO y , ice particle size distribution and total aerosol surface area. The measurements were performed in 2000 during the INCA campaign at northern and southern midlatitudes at local autumn. Cirrus ice particles were frequently encountered during these flights in the upper troposphere. Concurrently with the occurrence of cirrus ice particles particulate NO y was observed. It was found that the coverage of the cirrus ice particles with particulate NO y strongly depends on the temperature and the gas‐phase NO y concentration. A substantial coverage of the ice particles with values larger than one percent of a monolayer was observed only for temperatures below about 217 K. On average only about one percent of the available gas‐phase NO y was found as particulate NO y .