Helge F. Goessling coauthored work on the radiative response of the middle atmosphere to increased carbon dioxide. The paper develops a model perspective that distinguishes local emission and absorption from the whole-column energy budget.[ref]
It illustrates why the effect of changing an absorber cannot be inferred from its absorption strength alone. Optical depth, temperature and the surrounding radiation field jointly determine whether a layer gains or loses energy.
Articles by others on the same topic
There are currently no matching articles.