GEOG 2050 Chapter : GEOG2050 Oct 1
Document Summary
Which of the following do not change the shortwave radiation to longwave radiation (energy remains shortwave: diffusion, reflection, scattering, the earth has several mechanisms for heat transfer. Match the following: convective transfer-air circulation, direct heat loss-longwave radiation from earth"s surface, advection-horizontal convection, radiated from ozone layer-stratosphere, latent heat- evaporation, greenhouse effect- longwave radiation reflected back to. 2 f is within 90. 9 to 71. 9 f close to the average (81. 4 f) Above pink line or below its not with climatology average. Heat: energy of molecular movement, how fast they are actually moving, flow of energy. Temperature: amount of kinetic energy moved, bouncing off of something. Scattering: process of diffusion but you are getting diffuse radiation. Radiation: 110 but 96 but has greenhouse and has 14. Rayleigh scattering: blue at noon and red at night. Specific heat of water is the reason why the ocean does not heat up or cool down: water buffers the temp bc of high temperature heat.
