Answer. Between 6 p.m. on Nov. 10 and 6 a.m. on Nov. 11, the Norman temperature
profile cooled to the point where the whole vertical profile was below freezing at 6 a.m. If the Norman
sounding indicated moisture, the sounding would be a snow sounding. Because cold fronts slope towards
cold air (as seen here), the
depth of the cold air increases as the front moves past a given point. Thus, in our sounding, we can
see that as the front moved south past Norman, the depth of the cold air (seen through north winds and colder temperatures)
increased from 850 mb to 600 mb overnight.
|
OK-FIRST
Project, Oklahoma
Climatological Survey, 100 East
Boyd, Suite 1210, Norman, OK 73019
Copyright © 1996-2005 Oklahoma Climatological Survey. All
Rights Reserved.
Send comments or questions concerning OK-FIRST to
okfirst@mesonet.org
|