Ventura County, CA Flood Control, Watershed Modeling, and Watershed Management Studies
Client: Ventura County Watershed Protection District, Public Works Agency, Ventura, CA
The Ventura County Watershed Protection District (VCWPD), as owner and
operator of the receiving watercourses throughout the County, is
responsible for operation and maintenance of flood control facilities
and, under the county-wide NPDES permit, administration of the
stormwater quality program. To improve and expand its technical
procedures, VCWPD is exploring the use of continuous watershed
simulation as a tool for fulfilling its flood control, water resource
management, and water quality management obligations. Since June 2000
AQUA TERRA has been assisting the Ventura County Watershed Protection
District in its efforts to improve and expand its watershed assessment
procedures, through the use of continuous watershed simulation as a
tool for fulfilling its water resource management and water quality
management obligations. This assistance has occurred through a series
of individual projects described below.
Arroyo Simi Pilot Study
This project was a pilot study to evaluate the use of the
U.S. EPA Hydrologic Simulation Program FORTRAN (HSPF) as a management
tool for comprehensive watershed assessment within the climatic,
physiographic, and topographic conditions of Ventura County.
In the initial phase of the pilot study, HSPF was set up on the Arroyo
Simi watershed, and a preliminary hydrology calibration and validation
was performed on an eleven-year period of observed flows at two sites
within the watershed. The model results were presented in a Final
Report in 2001, and a presentation was made to Ventura County FCD,
along with a series of recommendations for future refinement of the
Arroyo Simi model calibration.
HSPF-VCRAT Comparison Study
In a follow-up effort to the Arroyo Simi model, the ‘preliminary’
calibration of the Arroyo Simi was used to compare HSPF model
predictions for flood peaks and volumes for various flood frequencies,
to those generated by the VCRAT method, a modified rational formula
approach previously used by VCWPD. Given that the HSPF model
calibration was not complete, the objective was not to assess how close
the two procedures agree, but rather to evaluate and compare the types
of flood assessment information generated by each approach. The flood
frequency comparisons of HSPF, VCRAT and the historic data show
reasonable agreement (see probability plot on following page). We also
explored and demonstrated the additional types of information available
from the HSPF watershed model that would further assist
USEP and Hydromodification
To address water quality issues, VCWPD has developed a Stormwater
Quality Urban Impact Mitigation Plan (SQUIMP) at the request of the Los
Angeles
Regional Water Quality Control Board. The SQUIMP addresses storm water
pollution from new development and redevelopment in the private sector.
One listed requirement of the SQUIMP (as defined in NPDES Permit No
CAS004002) is that “The discharger shall control the post-development
peak storm water runoff discharge rates to maintain or reduce
predevelopment downstream erosion, and to protect stream habitat.”
To respond to this requirement, VCWPD developed, in conjunction with
the LARWQCB, the Urban Stream Erosion Prevention Model (USEP) work plan
to address the issues of urbanization impacts on stream erosion and
habitat alteration. This effort extended the initial HSPF model setup
on the Arroyo Simi to include the specific habitat sites monitored in
USEP, finalized the preliminary hydrology calibration/validation, and
used the final model to assess stream erosive conditions under current,
natural and alternative scenarios for mitigation of urbanization
impacts. The objective was to develop and demonstrate procedures within
the Arroyo Simi watershed that might be applicable throughout the
County. The approach was to analyze the model-generated information on
flow and bed shear stress to determine how often (i.e., percent of
time) channel scour/erosion conditions occur. Specifically, the
calculated shear stress timeseries values were analyzed to determine
how often the values exceeded critical values for channel scour (tau
ratios of 1.5 and 2.5, see figure); this analysis established the
potential for channel scour conditions at any point within the
watershed.
Both current/baseline and scenario results were analyzed in a similar
fashion, so that urbanization impacts could be identified and
evaluated. The methodology assessed how often (i.e. what percent of
time) scour/deposition conditions occurred under each scenario, with
the differences from natural conditions representing the urbanization
impacts, and the differences for detention scenarios representing
mitigation impacts. Duration (cumulative frequency) curves were used to
analyze results for flow rate, velocity, and shear stress; shear stress
values were compared to ‘critical shear values’ for scour and
deposition to assess the frequency, duration, and ‘percent of time’ for
scour/deposition conditions. Also, flood statistics (e.g. 100-year,
50-year, 25-year, 10-year peak flows) were generated for each scenario
using accepted standard statistical procedures for flood analysis (e.g.
Log Pearson III), to assess scenario impacts on flood events along with
changes in the time duration of erosive conditions.
In January 2005 the California Regional Water Quality Control Board
(Los Angeles Region), recognizing the value of the approach, adopted
Resolution No. 2005-002 to provide a regional policy for
hydromodification analyses:
“…..The Regional Board and local agencies have undertaken or sponsored
hydro- modification field assessments and studies to develop peak flow
design criteria to minimize or eliminate adverse impacts form
urbanization for watercourses. These studies include the ‘Urbanization
and Channel Stability Assessment in the Arroyo Simi Watershed of
Ventura County, CA…. The results will be used to develop objective
criteria to reduce or eliminate the adverse impacts of
hydromodification in the Los Angeles Region from new development and
redevelopment.”
Calleguas Creek Watershed Study
The Arroyo Simi work efforts were extended downstream in this study to
develop a comprehensive watershed hydrologic model of the entire
Calleguas Creek Watershed, from its origins in the Arroyo Simi to its
discharge to Mugu Lagoon and the Pacific Ocean. This effort was jointly
funded by the Calleguas Creek Watershed Management Plan and the Ventura
County Watershed Protection District (VCWPD). HSPF was set up and
calibrated to available flow records for recent hydrologic conditions,
and customized to include consideration of localized groundwater
pumping impacts and lawn/landscape and agricultural irrigation
practices on surface water flow levels.
The Calleguas Creek Watershed covers an area of 340 sq. mi. and is
surrounded to the north, east, and south by largely undeveloped hills
and canyons, while the main stem flows through flat valleys consisting
of a mixture of urban and agricultural land. The goal was to develop a
watershed-wide hydrologic assessment tool. The watershed is subject to
flooding and erosion, resulting in sediment deposition downstream in
Mugu Lagoon. Topographic, soils, land use, and agricultural cropping
information were used to develop the model segmentation and input, and
detailed streamflow data were selected to allow calibration over a 9
year period (WY 1994 – WY 2002) and validation over a separate 6 year
period (WY 1988 – WY1993). Both quantitative and qualitative
comparisons were performed to support the model performance evaluation
effort.
Santa Clara River Feasibility Study and HSPF Model
AQUA TERRA has recently completed a major effort for Ventura County
that extends their HSPF modeling to the Santa Clara River watershed,
the neighboring watershed to Calleguas Creek. The new project is part
of the ongoing Santa Clara River (SCR) Watershed Feasibility Study
being undertaken jointly by VCWPD, Los Angeles Department of Public
Works, and the LA District of the U.S Army COE (USACE). In this effort
a ‘Baseline’ hydrologic model was developed with HSPF through model
setup, calibration, and validation with existing climatic data,
soil/watershed information, and hydrologic data for the SCR Watershed.
In addition, the model is being used to simulate extreme (i.e. 100-year
events), and long-term flow records at various locations in both
counties under Baseline, Natural, and Future Conditions. In the future,
it will be used for water quality simulations as described in the 2003
Project Management Plan.