101 Calendar

101 Home

Text & Office

Metacrawler

Grid Maps

 

EarthAlert

News

 

Atmosphere

Biosphere

Lithosphere

Earth Sciences

 

UWSP Geo Dept

UWSP Campus

 

 

Change Colors

 

 

 

 

 

 

 

 

 

 

 

 

 

 

 

 

 

 

 

Energy & Heat

Atmospheric "Windows"

  • Composition (variable gases) allow visible light in, but impede outgoing heat


Electromagnetic Spectrum

Atmosphere transmits much light (emitted by sun) to ground surface, which either absorbs or reflects it


Matter-Energy Interactions

Atmospheric heating primarily by shortwave light to ground, and longwave heat sent out from ground.


Atmospheric Heating

More specifically, atmosphere is about 70% heated from ground.

  • This is why the air should be warmest near the ground (nearest the primary heat source) under ordinary circumstances.


Atmospheric Energy Balance


Yours is visit # to this Web page since 10MAY97.

N. C. Heywood (nheywood@uwsp.edu) maintains this page, last updated 02SEP98.