Notes
Outline
Lecture 2: Global Energy Cycle
Solar Flux and Flux Density
 Solar Luminosity (L)
     the constant flux of energy put out by the sun
                         L = 3.9 x 1026   W
 Solar Flux Density (Sd)
     the amount of solar energy per unit area on a sphere centered at the Sun with a distance d
                         Sd  = L / (4 p d2)   W/m2
Solar Flux Density Reaching Earth
 Solar Constant (S)
    The solar energy density at the mean distance of      Earth from the sun (1.5  x 1011 m)
        S = L / (4 p d2)
           = (3.9 x 1026 W) / [4 x 3.14 x (1.5  x 1011 m)2]
           = 1370 W/m2
Solar Energy Incident On the Earth
 Solar energy incident on the Earth
      =  total amount of solar energy can be absorbed by Earth
      =  (Solar constant) x (Shadow Area)
      =  S x p R2Earth
Solar Energy Absorbed by Earth
What Happens After the Earth Absorbs Solar Energy?
 The Earth warms up and has to emit radiative  energy back to the space to reach a equilibrium condition.
 The radiation emitted by the Earth is called “terrestrial radiation” which is assumed to be like blackbody radiation.
Blackbody Radiation
 Blackbody
    A blackbody is something that emits (or absorbs) electromagnetic radiation with 100% efficiency at all wavelength.
 Blackbody Radiation
     The amount of the radiation emitted by a blackbody depends on the absolute temperature of the blackbody.
Energy Emitted from Earth
Planetary Energy Balance
Greenhouse Effect
Different Wavelengths of Solar and Earth’s Radiation
Greenhouse Gases
Earth, Mars, and Venus
Three Factors To Determine
 Planet Temperature
 Distance from the Sun
 Albedo
 Greenhouse effect
Global Temperature
Greenhouse Effects
 On Venus è 510°K (very large!!)
 On Earth   è 33°K
 On Mars   è 6°K (very small)
Why Large Greenhouse Effect On Venus?
 Venus is too close to the Sun
 Venus temperature is very high
 Very difficult for Venus’s atmosphere to get saturated in water vapor
 Evaporation keep on bringing water vapor into Venus’s atmosphere
 Greenhouse effect is very large
 A “run away” greenhouse happened on Venus
 Water vapor is dissociated into hydrogen and oxygen
 Hydrogen then escaped to space and oxygen reacted with carbon to form carbon dioxide
 No water left on Venus (and no more chemical weathering)
Why Small Greenhouse Effect on Mars?
 Mars is too small in size
Mars had no large internal heat
Mars lost all the internal heat quickly
No tectonic activity on Mars
Carbon can not be injected back to the atmosphere
Little greenhouse effect
A very cold Mars!!
Where Does the Solar Energy Go?
Where Is Earth’s Radiation Emitted From?
Important Roles of Clouds In Global Climate
Polarward Energy Transport
How Do Atmosphere and Ocean Transport Heat?