WW2010
University of Illinois

WW2010
 
welcome
 
online guides
 
archives
 
educational cd-rom
 
current weather
 
about ww2010
 
index

Online Guides
 
introduction
 
meteorology
 
remote sensing
 
reading maps
 
projects, activities

Meteorology
 
introduction
 
air masses, fronts
 
clouds, precipitation
 
el nino
 
forces, winds
 
hurricanes
 
hydrologic cycle
 
light, optics
 
midlatitude cyclones
 
severe storms
 
weather forecasting

Light, Optics
 
introduction
 
mechanisms
 
air, dust, haze
 
ice crystals
 
water droplets

water droplets
 
coronas
 
linings, iridescence
 
rainbows

User Interface
 
graphics
text

.
Silver Lining and Cloud Iridescence
produced through diffraction of sunlight

In the picture below, the sun is shining from behind the growing cumulus tower. This bright outline along the edge of the cloud is the silver lining, which occurs when light is diffracted by cloud droplets along the cloud's outer edge. Silver linings are observed around thicker clouds containing larger droplets.

[Image: photograph of silver lining (68K)]
Photograph by: Holle

Sometimes, diffraction of sunlight in clouds produce a multitude of colors. This optical effect is called cloud iridescence.

[Image: photograph of cloud iridescence (67K)]
Photograph by: Knupp

These colors are usually observed within 20 degrees of the sun and are easier to look at through sunglasses.



coronas
Terms for using data resources. CD-ROM available.
Credits and Acknowledgments for WW2010.
Department of Atmospheric Sciences (DAS) at
the University of Illinois at Urbana-Champaign.

Rainbows