1. Spectrum of terrestrial infrared radiation (Sportisse 2010).
Spectrum of terrestrial infrared radiation (Sportisse 2010). The spectrum is computed by the numerical model MODTRAN for the standard atmosphere (USA 1976, clear sky). The Planck black-body emission distributions are given for 220, 240, 260, 280 and 300 K. The corresponding greenhouse gases are indicated near the absorption peaks. This figure, from Sportisse (2010, fig. 2.12), is reproduced with permission © Springer.
Philip S. Ringrose Petroleum Geoscience 2017;23:
© 2017 The Author(s)‏