HomeMy WebLinkAbout3338; Agua Hedionda & Calavera Creek Dredging; Flood Control; 1996-11-104. Howard H. Chang Consultants
Hydraulic, Hydrologic and Sedimentation Engineering
P.O. Box 9492
Rancho Santa Fe, CA 92067
(619)756-9050,594-6380. FAX: (619)756-9460 *) i I
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November 10, 1996
Mr. Lee Anderson
Ms. Sue Loftin
Mr. Steve Weed
Rancho Carlsbad Country Club Estate
5200 El Camino Real
Carlsbad, California 92008
4,. Dear Friends:
Subject: Technical Review for the Hydraulic Study of Agua Hedionda Creek
by Ensign & Buckley in 1992
Pursuant to your request, I have reviewed the hydraulic study for Agua Hedionda Creek
in the City of Carlsbad made by Ensign & Buckley in 1992. The hydraulic study was for the
purpose of determining the 100-yr flood level and floodplain and floodway boundaries. My
review was to assess the accuracy of the study results for Agua Hedionda Creek at Rancho
Carlsbad Country Club.
In the review, I have found some basic mistakes in the study. Such mistakes resulted in
significantly higher 1Wyr flood elevations in Agua Hedionda Creek near El Camino Real. The
major mistakes include incorrect roughness coefficients, incorrect definitions of the main channel
and overbank areas, and improper split flow analysis to account for weir flows over the roadway
of El Camino Real as described below.
Incorrect roughness coefficients (or n value) were used for certain cross sections. For
exampie, the n value of 0.08 was used for the cross section just downstream of El Camino Real.
The NC record for this section is as follows:
NC 0.04 0.05 0.08 0.3 0.5
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This data record defms the n value of 0.04 for the left overbank, 0.05 for the right bank, and
0.08 for the main channel. The X1 record defines the main channel to be from station 25 feet to
170 feet for a total width of 145 feet. In fact, the main channel at this location has a bed width
of about 100 feet. The channel bed is basically free of vegetation but trees do grow near the
channel bank. Figure 1 shows physical conditions of the channel as viewed from the El Camino
Real Bridge. This picture was taken in the summer of 1996. Since the main channel is clean, the
proper n value should be about 0.03 but not the value of 0.08 used in the Ensign & Buckley study.
The incorrect definitions of the main channel and roughness coefficient contributed to a
significantly higher water-surface elevations near El Camino Real Bridge. Because of the higher
water-surface elevations, there would also be significant flood discharge overtopping the roadway
of El Camino Real. Most of the overtopping discharge would occur on the west side of the
channel where the roadway elevations are lower.
If correct n values had been used in Ensign & Buckley study, computed water-surface
elevations would have been lower and the overtopping discharge would have been much less and
most likely insignificant. At this time, the Cannon Road project is moving forward. After the
completion of Cannon Road, the overtopping flow to the west will be blocked by the higher road
embankment. As a conservative measure, one should disregard the overtopping flow in the
hydraulic computation. Without split flow due to overtopping, the starting water-surface elevation
at the downstream lit of study would also be lower according to the Ensign & Buckley study.
In conclusion, I have found some basic mistakes in the Ensign & Buckley study. Such
mistakes contributed to significantly higher 100-yr flood elevations near El Camino Real. In view
of the mistakes, it is necessary to revise the study before any official floodplain mapping is
adopted by the city of Carlsbad and FEh4.4.
Please free to call me if you have any questions regarding this matter.
I W.D., P.E.
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Fig. 1. View of main channel for Agua Hedionda Creek just downstream of El Camino Real
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.I -. . .. stud?. Even chough the precipitation-frequency maps pre:sen;d arc
prCphred considering physiographic facton. only those of a m+x
scale could be considerd. There are some basins. thercfore. that
are more sheltcrcd or uxpod than a generalized topographic map
would indicatc. The dup valucs may not be represellalive of thc
precipiration regimes in rgL'h basins.
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