Direct satellite observation of lightning-produced NO<sub>x</sub>

Lightning is an important source of NO<sub>x</sub> in the free troposphere, especially in the tropics, with strong impact on ozone production. However, estimates of lightning NO<sub>x</sub> (LNO<sub>x</sub>) production efficiency (LNO<sub>x</sub> pe...

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Main Authors: T. Wagner, H. Huntrieser, S. Beirle
Format: Article
Language:English
Published: Copernicus Publications 2010-11-01
Series:Atmospheric Chemistry and Physics
Online Access:http://www.atmos-chem-phys.net/10/10965/2010/acp-10-10965-2010.pdf
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spelling doaj-97208e2fccb141b6a4f6273af611048f2020-11-24T22:56:04ZengCopernicus PublicationsAtmospheric Chemistry and Physics1680-73161680-73242010-11-011022109651098610.5194/acp-10-10965-2010Direct satellite observation of lightning-produced NO<sub>x</sub>T. WagnerH. HuntrieserS. BeirleLightning is an important source of NO<sub>x</sub> in the free troposphere, especially in the tropics, with strong impact on ozone production. However, estimates of lightning NO<sub>x</sub> (LNO<sub>x</sub>) production efficiency (LNO<sub>x</sub> per flash) are still quite uncertain. <br><br> In this study we present a systematic analysis of NO<sub>2</sub> column densities from SCIAMACHY measurements over active thunderstorms, as detected by the World-Wide Lightning Location Network (WWLLN), where the WWLLN detection efficiency was estimated using the flash climatology of the satellite lightning sensors LIS/OTD. Only events with high lightning activity are considered, where corrected WWLLN flash rate densities inside the satellite pixel within the last hour are above 1 /km<sup>2</sup>/h. For typical SCIAMACHY ground pixels of 30 × 60 km<sup>2</sup>, this threshold corresponds to 1800 flashes over the last hour, which, for literature estimates of lightning NO<sub>x</sub> production, should result in clearly enhanced NO<sub>2</sub> column densities. <br><br> From 2004–2008, we find 287 coincidences of SCIAMACHY measurements and high WWLLN flash rate densities. For some of these events, a clear enhancement of column densities of NO<sub>2</sub> could be observed, indeed. But overall, the measured column densities are below the expected values by more than one order of magnitude, and in most of the cases, no enhanced NO<sub>2</sub> could be found at all. <br><br> Our results are in contradiction to the currently accepted range of LNO<sub>x</sub> production per flash of 15 (2–40)&times;10<sup>25</sup> molec/flash. This probably partly results from the specific conditions for the events under investigation, i.e. events of high lightning activity in the morning (local time) and mostly (for 162 out of 287 events) over ocean. <br><br> Within the detected coincidences, the highest NO<sub>2</sub> column densities were observed around the US Eastcoast. This might be partly due to interference with ground sources of NO<sub>x</sub> being uplifted by the convective systems. However, it could also indicate that flashes in this region are particularly productive. <br><br> We conclude that current estimates of LNO<sub>x</sub> production might be biased high for two reasons. First, we observe a high variability of NO<sub>2</sub> for coincident lightning events. This high variability can easily cause a publication bias, since studies reporting on high NO<sub>x</sub> production have likely been published, while studies finding no or low amounts of NO<sub>x</sub> might have been rejected as errorneous or not significant. Second, many estimates of LNO<sub>x</sub> production in literature have been performed over the US, which is probably not representative for global lightning. http://www.atmos-chem-phys.net/10/10965/2010/acp-10-10965-2010.pdf
collection DOAJ
language English
format Article
sources DOAJ
author T. Wagner
H. Huntrieser
S. Beirle
spellingShingle T. Wagner
H. Huntrieser
S. Beirle
Direct satellite observation of lightning-produced NO<sub>x</sub>
Atmospheric Chemistry and Physics
author_facet T. Wagner
H. Huntrieser
S. Beirle
author_sort T. Wagner
title Direct satellite observation of lightning-produced NO<sub>x</sub>
title_short Direct satellite observation of lightning-produced NO<sub>x</sub>
title_full Direct satellite observation of lightning-produced NO<sub>x</sub>
title_fullStr Direct satellite observation of lightning-produced NO<sub>x</sub>
title_full_unstemmed Direct satellite observation of lightning-produced NO<sub>x</sub>
title_sort direct satellite observation of lightning-produced no<sub>x</sub>
publisher Copernicus Publications
series Atmospheric Chemistry and Physics
issn 1680-7316
1680-7324
publishDate 2010-11-01
description Lightning is an important source of NO<sub>x</sub> in the free troposphere, especially in the tropics, with strong impact on ozone production. However, estimates of lightning NO<sub>x</sub> (LNO<sub>x</sub>) production efficiency (LNO<sub>x</sub> per flash) are still quite uncertain. <br><br> In this study we present a systematic analysis of NO<sub>2</sub> column densities from SCIAMACHY measurements over active thunderstorms, as detected by the World-Wide Lightning Location Network (WWLLN), where the WWLLN detection efficiency was estimated using the flash climatology of the satellite lightning sensors LIS/OTD. Only events with high lightning activity are considered, where corrected WWLLN flash rate densities inside the satellite pixel within the last hour are above 1 /km<sup>2</sup>/h. For typical SCIAMACHY ground pixels of 30 × 60 km<sup>2</sup>, this threshold corresponds to 1800 flashes over the last hour, which, for literature estimates of lightning NO<sub>x</sub> production, should result in clearly enhanced NO<sub>2</sub> column densities. <br><br> From 2004–2008, we find 287 coincidences of SCIAMACHY measurements and high WWLLN flash rate densities. For some of these events, a clear enhancement of column densities of NO<sub>2</sub> could be observed, indeed. But overall, the measured column densities are below the expected values by more than one order of magnitude, and in most of the cases, no enhanced NO<sub>2</sub> could be found at all. <br><br> Our results are in contradiction to the currently accepted range of LNO<sub>x</sub> production per flash of 15 (2–40)&times;10<sup>25</sup> molec/flash. This probably partly results from the specific conditions for the events under investigation, i.e. events of high lightning activity in the morning (local time) and mostly (for 162 out of 287 events) over ocean. <br><br> Within the detected coincidences, the highest NO<sub>2</sub> column densities were observed around the US Eastcoast. This might be partly due to interference with ground sources of NO<sub>x</sub> being uplifted by the convective systems. However, it could also indicate that flashes in this region are particularly productive. <br><br> We conclude that current estimates of LNO<sub>x</sub> production might be biased high for two reasons. First, we observe a high variability of NO<sub>2</sub> for coincident lightning events. This high variability can easily cause a publication bias, since studies reporting on high NO<sub>x</sub> production have likely been published, while studies finding no or low amounts of NO<sub>x</sub> might have been rejected as errorneous or not significant. Second, many estimates of LNO<sub>x</sub> production in literature have been performed over the US, which is probably not representative for global lightning.
url http://www.atmos-chem-phys.net/10/10965/2010/acp-10-10965-2010.pdf
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