The photolysis of chlorine nitrate was studied using broadband flash photolysis coupled with long-path ultraviolet-visible absorption spectroscopy. Branching ratios for the Cl + NO 3 and ClO + NO 2 product channels were determined from time-dependent measurements of ClO and NO 3 concentrations. Yields of the ClO and NO 3 products displayed a dependence on the bath gas density and the spectral distribution of the photolysis pulse. Product yields decreased with increasing bath gas density regardless of the spectral distribution of the photolysis pulse; however, the decrease in product yield was much more pronounced when photolysis was limited to longer wavelengths. For photolysis in a quartz cell (λ > 200 nm) the yield decreased by a factor of 2 over the pressure 10-100 Torr. In a Pyrex cell (λ > 300 nm), the yield decreased by a factor of 50 over the same pressure range. When photolysis was limited to λ > 350 nm, the yield decreased by a factor of 250. Branching ratios for the photolysis channels [ClONO 2 + hν f ClO + NO 2 (1a) and ClONO 2 + hν f Cl + NO 3 (1b)] were determined from the relative ClO and NO 3 product yields at various pressures. Although the absolute product yield displayed a pressure dependence, the branching between the two channels was independent of pressure. The relative branching ratios (assuming negligible contributions from other channels) are 0.61 ( 0.20 for channel 1a and 0.39 ( 0.20 for channel 1b for photolysis with λ > 200 nm and 0.44 ( 0.08 for channel 1a and 0.56 ( 0.08 for channel 1b for photolysis with λ > 300 nm. The implications of these results for the chemistry of the lower stratosphere are discussed.