[摘要] Nitrogen oxides (NO
xNO+NO
2) play an important role intropospheric chemistry, in particular in catalytic ozone production.Lightning provides a natural source of nitrogen oxides, dominating theproduction in the tropical upper troposphere, with strong impact ontropospheric ozone and the atmosphere's oxidizing capacity. Recent estimatesof lightning produced NO
x (LNO
x) are of the order of 5 Tg [N] peryear with still high uncertainties in the range of one order of magnitude.
The Global Ozone Monitoring Experiment (GOME) on board the ESA-satelliteERS-2 allows the retrieval of tropospheric column densities of NO2 on aglobal scale. Here we present the GOME NO2 measurement directly over alarge convective system over the Gulf of Mexico. Simultaneously,cloud-to-ground (CG) flashes are counted by the U.S. National LightningDetection Network (NLDNTM), and extrapolated to includeintra-cloud (IC)+CG flashes based on a climatological IC:CG ratio derivedfrom NASA's space-based lightning sensors. A series of 14 GOME pixels showslargely enhanced column densities over thick and high clouds, coincidingwith strong lightning activity. The enhancements can not be explained bytransport of anthropogenic NOx and must be due to fresh production of LNOx. A quantitative analysis, accounting in particular for thevisibility of LNOx from satellite, yields a LNOx production of 90(32-240) moles of NOx, or 1.3 (0.4-3.4) kg [N], per flash. If simplyextrapolated, this corresponds to a global LNOx production of 1.7(0.6-4.7)Tg [N]/yr.