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

Reading Maps
 
introduction
 
utc conversions
 
temp conversions
 
surface obs
 
surface maps
 
upper air obs

Surface Obs
 
overview
 
temperature
 
weather
 
dew points
 
cloud cover
 
pressure
 
winds
 
contours

Contours
 
introduction
 
isobars
 
wind & isobars
 
isotherms
 
isodrosotherms
 
more contouring

User Interface
 
graphics
text

.
Contouring
surface maps

Sometimes the reported values (black numbers) are not always located between the correct contours. For example, in the dew point temperature map below, a station in Minnesota (circled in blue) reported a dew point temperature of 52 degrees, but it is located between the 60 and 65 degree contours.

Why is this so? Because contours are plotted to provide a "best-fit" for all reports, which include a very large number of stations. To give you an idea, I've increased the number of reporting stations in the image below.

This is the exact same dew point map, but with many more station reports (black numbers). And this still doesn't include all of them!

In order for every station to be within the correct contours, lines would be zigging and zagging everywhere, making the map unreadable. Fortunately, contour lines are smoothed to make the map readable.

Therefore, it is important to remember that although the contours may not be 100% accurate for every single reporting station, contouring provides READABLE information, as accurately as possible, for a HUGE number of reporting stations.



isodrosotherms
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.

Temperature Maps