ATMOSPHERIC RADICAL PRODUCTION BY EXCITATION OF VIBRATIONAL OVERTONESVIA ABSORPTION OF VISIBLE-LIGHT

We present calculations using a radiative transfer model which predict that in the lower stratosphere at high zenith angles, significant enh ancements to the photodissociation rates of HNO3 and HNO4 can result f rom visible wavelength excitation of OH overtone vibrations containing sufficient energy to cleave the O-O and N-O bonds. The results indica te that atmospheric chromophores such as HONO2. HO2NO2 and H2O2, could make a potentially significant contribution to the production of HOx and NOx. Calculating the relative importance of their effect requires better knowledge of the absolute absorption cross sections: both for v ibrational overtones and in the near UV. Stratospheric air masses in w hich this process could be important are those that experience lengthy exposure at high solar zenith angles: the outer regions of the polar winter vortex and the polar summer anticyclone. We note that the gener al mechanism may have application elsewhere such as in the atmospheres of other planets and in generating the diffuse interstellar bands ass ociated with molecular clouds.