<p><strong>Abstract.</strong> Nitrogen oxides (NO<sub>x</sub>&#8201;&#8801;&#8201;NO&#8201;+&#8201;NO<sub>2</sub>) in the upper troposphere (UT) have a large impact on global tropospheric ozone and OH (the main atmospheric oxidant). New cloud-sliced observations of UT NO<sub>2</sub> at 450&#8211;280&#8201;hPa (~&#8201;6&#8211;9&#8201;km) from the OMI satellite instrument produced by NASA and KNMI provide global coverage to test our understanding of the factors controlling UT NO<sub>x</sub>. We find that these products offer useful information when averaged over coarse scales (20&#176;&#8201;&#215;&#8201;32&#176;, seasonal), and that the NASA product is more consistent with aircraft observations of UT NO<sub>2</sub>. Correlation with LIS/OTD satellite observations of lightning flash frequencies shows that lightning is the dominant source of NO<sub>x</sub> to the upper troposphere except for extratropical latitudes in winter. We infer a global mean NO<sub>x</sub> yield of 280 moles per lightning flash, with no significant difference between the tropics and mid-latitudes, and a global lightning NO<sub>x</sub> source of 5.6&#8201;Tg&#8201;N&#8201;a<sup>&#8722;1</sup>. There is indication that the NO<sub>x</sub> yield per flash increases with lightning flash footprint and with flash energy.</p>