<p><strong>Abstract.</strong> Both canopy-level field measurements and laboratory studies suggest that absorption of NO<sub>2</sub> through the leaf stomata of vegetation is a significant sink of atmospheric NO<sub><i>x</i></sub>. However, the mechanisms of this foliar NO<sub>2</sub> uptake and their impact on NO<sub><i>x</i></sub> lifetimes remains incompletely understood. To understand the leaf-level processes affecting ecosystem scale atmosphere-biosphere NO<sub><i>x</i></sub> exchange, we have conducted laboratory experiments of branch-level NO<sub>2</sub> deposition fluxes to six coniferous and four broadleaf native California trees using a branch enclosure system with direct Laser Induced Fluorescence (LIF) detection of NO<sub>2</sub>. We report NO<sub>2</sub> foliar deposition that demonstrates a large degree of inter-species variability, with maximum observed deposition velocities ranging from 0.15&#8211;0.51&#8201;cm/s during the daytime, as well as significant stomatal opening during the night. We also find that the contribution of mesophyllic processing to the overall deposition rate of NO<sub>2</sub> varies by tree species, but has an ultimately inconsequential impact on NO<sub><i>x</i></sub> budgets and lifetimes. Additionally, we find no evidence of any emission of NO<sub>2</sub> from leaves, suggesting an effective uni-directional exchange of NO<sub><i>x</i></sub> between the atmosphere and vegetation.</p>