A one-dimensional, time-dependent, photochemical model is used in conjunction with data obtained during the dry-season portion of NASA's Global Tropospheric Experiment and Brazil's Instituto Nacional de Pesquisas Espaciais (INPE) (National Institute for Space Research) Amazon Boundary Layer Experiment (ABLE 2A) to simulate the chemistry of the dry-season Amazon troposphere. The background atmosphere, unperturbed by the presence of emissions from biomass burning, is simulated with inputs of surface sources and deposition of various species measured during ABLE 2A. The presence of haze layers over a region is simulated by the imposition of profiles of species characteristics of haze within the model for 12 hours. The inclusion of hydrocarbons within the modeled haze is found to approximately double the calculated in situ ozone production rate. The difference between the calculated total column ozone production rates in the haze simulation of the background simulation is the model-predicted enhancement of the in situ ozone production due to regionally transported haze layers (up to 1000 km transport distance). The predicted enhancement of ozone is between 0.3 and 2.9¿1011 molecules O3 cm-2 s-1, near the range of observed rates of ozone increase over the Amazon Basin duirng the during the dry season. This suggests that the regional transport of haze during the southern tropical burning season is an importnat factor in explaining the increase of ozone observed annually during this period. ¿American Geophysical Union 1991