Using TES radiances, Jacobians and ozone profiles with hemispherical integration, it is possible to compute the TOA (top-of-atmosphere) flux from the infrared ozone band (in W/m2), instantaneous radiative kernels (IRK) (in W/m2/ppb), and logarithmic instantaneous radiative forcing kernels (LIRK) (in W/m2) for ozone. The IRK provides unique information for questions of chemistry-climate coupling since this is a direct measure of the radiative role of ozone which explicitly accounts for more dominant radiative processes such as clouds and water vapor. These products can be compared to climate model predictions of the same quantities.