TEMPERATURE-DEPENDENT OZONE TRANSMITTANCE IN A MONOLAYER ATMOSPHERIC MODEL

The need for information on spectral ozone transmittance arises from t he temperature-dependence of the ozone absorption coefficients in Hart ley-Huggins bands (200-360 nm). The methodological approach reported h ere employs the convolution between vertical profiles of ozone and tem perature to determine the ozone layer's effective temperature. Introdu cing temperature makes it possible better to approximate UV-spectral o zone transmittance values computed by LOWTRAN-7.