Open Access
In situ measurements of the NO x distribution and variability over the eastern North Atlantic
Author(s) -
Ziereis H.,
Schlager H.,
Schulte P.,
Köhler I.,
Marquardt R.,
Feigl C.
Publication year - 1999
Publication title -
journal of geophysical research: atmospheres
Language(s) - English
Resource type - Journals
SCImago Journal Rank - 1.67
H-Index - 298
eISSN - 2156-2202
pISSN - 0148-0227
DOI - 10.1029/1999jd900175
Subject(s) - stratosphere , troposphere , tropopause , atmospheric sciences , environmental science , climatology , atmosphere (unit) , altitude (triangle) , mixing ratio , geology , meteorology , geography , geometry , mathematics
Between 1994 and 1996 the research aircraft Falcon of the Deutsches Zentrum für Luft‐ und Raumfahrt was used to probe the upper troposphere and lowermost stratosphere over the eastern North Atlantic. In situ measurements of NO, NO 2 , and O 3 were performed during 32 flights. The measurements were carried out during five aircraft campaigns in summer and late autumn, respectively, based from Shannon, Ireland, and Prestwick, Scotland. Most of the flights were conducted in the region of the North Atlantic flight corridor. Main objectives of these measurements included the study of the large‐scale distribution of NO and NO x and the development of reliable monthly mean values for different seasons in a region of the atmosphere that is strongly affected by aircraft emissions. Substantial variability of NO and NO x volume mixing ratios was observed in the upper troposphere and lowermost stratosphere. In spite of this variability a significant seasonal dependence was found. NO mean values (averages over all measurements made during one campaign) at altitudes between 10,500 and 11,500 m, where most of the data have been obtained, ranged between about 0.1 and 0.14 ppbv in summer and 0.03 and 0.10 ppbv in late autumn. NO and NO x did not show a significant gradient across the tropopause. The correlation between NO x and O 3 in the upper troposphere and lowermost stratosphere was only very weak. The present measurements represent a suitable data set for comparison with predictions of the NO x distribution in the upper troposphere over the eastern North Atlantic by three‐dimensional models. A comparison with the NO x fields simulated with the European Center for Medium‐Range Weather Forecasts, Hamburg Version 3 (ECHAM 3) climate model extended by a simplified NO x chemistry reveals good agreement for summer and autumn conditions.