Direct measurements of ozone and nitrogen dioxide photolysis rates in the troposphere

The photolysis frequencies of ozone and nitrogen dioxide were measured under a variety of conditions commonly found in the troposphere. Ozone photolysis frequencies show a strong dependence on solar zenith angle, overhead ozone column, and temperature, but only a weak dependence on altitude (when only downward radiation is detected). Nitrogen dioxide photolysis frequencies also show strong dependence on solar zenith angle, but show little dependence on temperature, pressure, or altitude. Both j values are strongly affected by cloud cover, but aerosol loading has much less effect. The disagreement of measured j(O3) and j(NO2) with many modeled values, especially disagreement over altitude dependence, shows that atmospheric UV radioactive processes are complicated and poorly understood, although experimental conditions may not always be applicable to conditions modeled.