An update on reactive odd‐nitrogen measurements made during recent NASA Global Tropospheric Experiment programs

This report addresses issues that have been raised recently about the measurements of reactive odd nitrogen and, in particular, those measurements made as part of the NASA Global Tropospheric Experiment airborne field campaigns. The test results presented here demonstrate that it is unlikely that HNO 3 mixing ratios are underestimated by large factors (i.e., by greater than 1.5‐fold) during the Pacific Exploratory Mission‐ West A, Transport and Atmospheric Chemistry Near the Equator Atlantic, and Pacific Exploratory Mission‐ West B field campaigns and that other mechanisms are needed to explain discrepancies between measured and modeled HNO 3 mixing ratios. Results from NO y conversion efficiency studies indicate that potentially large artifacts may have affected the Georgia Institute of Technology measurements of total reactive odd nitrogen (NO y ). Assessing the exact magnitude of these artifacts is hindered by a lack of knowledge of both tropospheric distributions of non‐NO y forms of fixed nitrogen and the efficiency with which they were detected at the time of the NO y measurement. Indirectly, our results suggest that up to ppbv levels of non‐NO y fixed nitrogen (e.g., NH 3 , HCN, and perhaps nitrogeneous sulfur compounds) may exist in some regions of the remote troposphere.