The chemical NOx budget in the upper troposphere over the tropical South Pa
cific is analyzed using aircraft measurements made at 6-12 km altitude in S
eptember 1995 during the Global Tropospheric Experiment (GTE) Pacific Explo
ratory Mission (PEM) Tropics A campaign. Chemical loss and production rates
of NOx along the aircraft flight tracks are calculated with a photochemica
l model constrained by observations. Calculations using a standard chemical
mechanism show a large missing source for NOx; chemical loss exceeds chemi
cal production by a factor of 2.4 on average. Similar or greater NOx budget
imbalances have been reported in analyses of data from previous field stud
ies. Ammonium aerosol concentrations in PEM-Tropics A generally exceeded su
lfate on a charge equivalent basis, and relative humidities were low (media
n 25% relative to ice). This implies that the aerosol could be dry in which
case N2O5 hydrolysis would be suppressed as a sink for NOx. Suppression of
N2O5 hydrolysis and adoption of new measurements of the reaction rate cons
tants for NO2 + OH + M and HNO3 + OH reduces the median chemical imbalance
in the N-x budget for PEM-Tropics A from 2.4 to 1.9. The remaining imbalanc
e cannot be easily explained from known chemistry or long-range transport o
f primary NOx and may imply a major gap in our understanding of the chemica
l cycling of NOx in the free troposphere.