Page 303 - Ultimate Visual Dictionary (DK)
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THE ATMOSPHERE

                                                       STRUCTURE OF THE           GLOBAL WARMING
                                                       ATMOSPHERE
                                                                      Solar radiation    Some reradiated
                                                                      reradiated as heat  heat escapes
                                                                                         into space
                                                                       Sun
                                                                                              Some reradiated
                                                                                             heat reflected back
                                                                                                    to Earth
                                                                   Incoming solar
                                                                   radiation
                                                                                                     Earth
                                                                     Atmosphere


                                                                                 NATURALLY MODERATED
                                                                                  GREENHOUSE EFFECT
                                                                   Meteor (shooting star)
                                                                   burns up as it passes   Less reradiated
                                                                   through atmosphere    heat escapes
                                                                       Solar radiation       More reradiated
                                                                       reradiated as heat    heat reflected
                                                                                             back to Earth
                                                                                                 Surface
                                                                Aurora
                                                                                                 temperature
                                                                                                 rises
                                                                 “Greenhouse
                                                                 gases” accumulate
                                                                 in atmosphere


                                                             Incoming solar
                                                             radiation
                                                                                UNBALANCED GREENHOUSE
                                                           14% of  incoming solar      EFFECT
                                                           radiation absorbed
                                                           by atmosphere
                                                          7% of  incoming solar   COMPOSITION OF THE
                                                          radiation reflected      LOWER ATMOSPHERE
                                                          by atmosphere
                                                                                    Other elements less
                                                                                    than 0.1%
                                                             24% of  incoming
                                                             solar radiation                     Argon 0.93%
                                                             reflected by clouds
                                                                 Cosmic rays (high-energy       Oxygen 21%
                                                                 particles from space)
                                                                 penetrate to stratosphere
                                                                     Some absorbed
                                                                     heat reradiated
                                                                     by atmosphere               Nitrogen 78%
                                                                    4% of  incoming solar
                                                                    radiation reflected by
                                                                    oceans and land
                                                                    51% of  incoming solar
                                                                    radiation absorbed by
                                                                    Earth’s surface
                                                                    Some absorbed heat
                                                                    re-radiated by clouds

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