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EARTH'S RADIATION & ENERGY BALANCE

 

A. INTRODUCTION

1. Energy

2. Calorie


B. FORMS OF ENERGY
link icon: note about textbook link icon: note about textbook

1. Radiant Energy (electromagnetic radiation)

temperature of a substance affects:

  • wavelength of radiation emitted

  • intensity (amount) of radiation emitted link icon: information on inifrared (longwave) radiation

solar radiation and terrestrial radiation:

diagram: solar & terrestrial radiation spectra

diagram: water phase changes

 

2. Heat (thermal) Energy

a. temperature and heat

b. specific heat and heat capacity

c. forms of heat energy



C. RADIATION BALANCE
link icon: note about textbook

1. Net radiation = total in - total out

image: radiation balance equation

2. Shortwave (solar) radiation  (K)    

incoming shortwave

  • image: incoming shortwave radiation= (S+D)

  • direct beam solar (S)

  • diffuse (scattered) solar (D)

outgoing shortwave

  • reflected radiation

  • image: outgoing shortwave radiation= [a(S+D)]

  • albedo: proportion of insolation reflected from a surface (a)

  • insolation reflected by atmosphere & earth's surface

  • albedo varies geographically & temporally

link icon: January albedo link icon: July albedo

diagram: shortwave radiation fluxes

Maps of image: incoming shortwave radiation
maps: global insolation in january and april
Image source: NASA Visible Earth http://visibleearth.nasa.gov/view_rec.php?id=1683

net shortwave

3. Longwave (terrestrial) radiation            

incoming longwave

  • image: incoming longwave radiation

  • radiation emitted by atmosphere

  • function of air temperature

outgoing longwave

  • image: outgoing longwave radiation

  • radiation emitted by earth

  • function of surface temperature

net longwave

  • image: net longwave radiation equation

  • earth's surface and atmosphere absorb longwave radiation

link icon: january outgoing longwave radiation link icon: july outgoing longwave radiation link icon: animation of outgoing longwave radiation

diagram: longwave radiation fluxes

4. Radiation balance summary

net radiation = amount radiant energy available to do work

net radiation = total in - total out


D. ENERGY BALANCE

1. Energy always transferred from warmer to cooler substances

2. Mechanisms:diagram: energy fluxes

Picture (262x27, 1.5Kb)

graph: monthly energy fluxes for West Palm Beach graph: monthly energy fluxes for Yuma


E. SUMMARY

image: radiation & energy balance equations

Temperature patterns affected by:

link icon: animation of air temperature


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© Karen A. Lemke: klemke@uwsp.edu
Last revised January 26, 2007