Recent urban measurements suggest that NO3 concentrations vary significantl
y with altitude in the lowest few hundred metres of the atmosphere. Calcula
tions using a one-dimensional boundary layer model show that NO3 concentrat
ions are small near the ground and increase with altitude to a maximum near
the top of the nocturnal boundary layer (NBL). These results show that the
NBL is not well mixed, and that where there are surface sources and sinks
two-box models of the NBL are inadequate, and surface measurements are not
representative and may lead to an underestimate of the oxidising capacity o
f the atmosphere. (C) 1999 Elsevier Science Ltd. All rights reserved.