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Measurements of reactive nitrogen produced by tropical thunderstorms during BIBLE-C

Authors :
N. Nishi
T. Ogawa
Kazuyuki Kita
S Kudoh
Yutaka Kondo
B. Liley
Yuzo Miyazaki
Malcolm K. W. Ko
T Kashihara
Donald R. Blake
Tomoko Shirai
Makoto Koike
Shuji Kawakami
Nobuyuki Takegawa
Zen Kawasaki
Source :
Journal of Geophysical Research. 112
Publication Year :
2007
Publisher :
American Geophysical Union (AGU), 2007.

Abstract

[1] The Biomass Burning and Lightning Experiment phase C (BIBLE-C) aircraft mission was carried out near Darwin, Australia (12°S, 131°E) in December 2000. This was the first aircraft experiment designed to estimate lightning NO production rates in the tropics, where production is considered to be most intense. During the two flights (flights 10 and 13 made on December 9 and 11–12, respectively) enhancements of NOx (NO + NO2) up to 1000 and 1600 parts per trillion by volume (pptv, 10-s data) were observed at altitudes between 11.5 and 14 km. The Geostationary Meteorological Satellite (GMS) cloud (brightness temperature) data and ground-based lightning measurements by the Global Positioning and Tracking System (GPATS) indicate that there were intensive lightning events over the coast of the Gulf of Carpentaria, which took place upstream from our measurement area 10 to 14 h prior to the measurements. For these two flights, air in which NOx exceeded 100 pptv extended over 620 × 140 and 400 × 170 km2 (wind direction × perpendicular direction), respectively, suggesting a significant impact of lightning NO production on NOx levels in the tropics. We estimate the amount of NOx observed between 11.5 and 14 km produced by the thunderstorms to be 3.3 and 1.8 × 1029 NO molecules for flights 10 and 13, respectively. By using the GPATS lightning flash count data, column NO production rates are estimated to be 1.9–4.4 and 21–49 × 1025 NO molecules per single flash for these two flight data sets. In these estimations, it is assumed that the column NO production between 0 and 16 km is greater than the observed values between 11.5 and 14 km by a factor of 3.2, which is derived using results reported by Pickering et al. (1998). There are however large uncertainties in the GPATS lightning data in this study and care must be made when the production rates are referred. Uncertainties in these estimates are discussed. The impact on the ozone production rate is also described.

Details

ISSN :
01480227
Volume :
112
Database :
OpenAIRE
Journal :
Journal of Geophysical Research
Accession number :
edsair.doi...........0f6e307e6641354fe4b755e93af8ceec
Full Text :
https://doi.org/10.1029/2006jd008193