[Acoustics] Questions:extrapolation methods and 3 beam solutions
Michael R Simpson
msimpson at usgs.gov
Tue Jul 8 14:31:13 CDT 2003
I'll try to answer the first one, and let someone else answer the three
beam question.
As you cross a typical channel, the depth will increase significantly at
some point and many times, the highest water velocity is found near the
deepest portion of the channel (but not always, and especially not on
curved reaches). In tidal channels, profiles near the edges may have a
non-standard shape. In channels having a salinity gradient, the velocity
profile shape may be significantly different than a standard logrithmic
profile (the bottom may be moving in a different direction than the top)
because of fluid density differences. Bottom roughness also plays a part
in the shape of the velocity profile. Wind may be affecting the surface
velocity on one side of the channel, but not the other. Averaging the
whole cross section would simply not provide an accurate picture of the
"average" velocity profile.
It would be really easy to simply say that a short average, taken in the
deepest, fastest part of the channel, where the depth does not vary too
much, would be an ideal sample for use in examining the velocity profile
shape. Maybe that would work in 75% of the cases, but what about the
other cases where the edge profiles are non-standard, or there exists
density gradients in only certain portions of the cross-section.
The answer is: There is no right answer that would cover all situations.
Bottom velocities most often roll off to zero, so that is not a bad
general assumption, but velocities near the surface are unpredictable.
Each case must be examined on its own merits and the proper profile chosen
based on common sense and the examination of all the collected data
(separated into different zones if need be.)
................................................................................
Michael R. Simpson
USGS
Placer Hall, 6000 J. Street
Sacramento, CA 95819-6129
(916) 278-3130 cel (916) 997-8048
................................................................................
" The wonderful thing about standards is that there are so many of them to
choose from" - Grace Murray Hopper
...............................................................................
"Thomas P Suro" <tsuro at usgs.gov>
Sent by: acoustics-admin at simon.er.usgs.gov
07/08/2003 12:14 PM
To: acoustics at simon.er.usgs.gov
cc:
Subject: [Acoustics] Questions:extrapolation methods and 3 beam solutions
I have two questions about how others are applying the new
extrapolation
methods and the use of 3 beam solution.
1. As the new OSW memo states, and I agree, we should not be using
constant on the bottom. OK, but my question is about choosing
between
constant and 3 pt. slope on the top and power and no slip on the
bottom. I usually average the entire transect and look at the
profile. Then I average it into three or four pieces and look at the
areas with the most flow (velocity). I some cases I will use the
method that looks best in the major flow areas instead of using the
entire transect average to pick the extrapolation method.
I know everyone has an opinion, but does anyone have any specific
reasoning to always average one way or another when picking an
extrapolation method?
Tom
====================
Thomas P. Suro
Hydrologist & Engineer
U.S. Geological Survey
425 Jordan Road
Troy, New York 12180
Tel: (518) 285-5642
Fax: (518) 285-5601
tsuro at usgs.gov
====================
_______________________________________________
Acoustics mailing list
Acoustics at simon.er.usgs.gov
http://il.water.usgs.gov/mailman/listinfo/acoustics
-------------- next part --------------
An HTML attachment was scrubbed...
URL: http://simon.er.usgs.gov/pipermail/acoustics/attachments/20030708/c3b3f6de/attachment-0001.html
More information about the Acoustics
mailing list