HomeMy WebLinkAbout014.07 - Appendix L.9 - Flood Study Waiver Memo MEADOW BRIDGE SUBDIVISION
Project #BOZ-05021.28
Bozeman, Montana
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Community Planning
Surveying+ Mapping+GIS+Drone
Civil Infrastructure Engineering MARCH 2O25
Multimodal Transportation
Engineering
Water and Wastewater Utility
Design and Operations
Landscape Architecture+
Placemaking
Construction Management and
Inspection
Communications+Public
Engagement+Visualizations
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MEMORANDUM
To: City of Bozeman Engineering Department - Floodplain
From: Bobby Egeberg, PE - Sanbell
Date: 3/6/2025
Reference: Meadow Bridge Subdivision Preliminary Plat - Floodplain
The purpose of this Memorandum is to provide existing floodplain information within the
proposed Meadow Bridge Subdivision Preliminary Plat currently under review with the City of
Bozeman, as well as request a waiver for additional Flood Study analysis as required in BMC
38.600.150.B. The Meadow Bridge Subdivision Preliminary Plat is located within Phases II & III of
Meadow Creek Subdivision which were partially constructed including utilities, ponds, curb &
gutter, and sections of asphalt paving. The development went bankrupt in the 2008 recession, and
construction was never completed. This portion Meadow Creek Subdivision is now proposed to be
subdivided and named the Meadow Bridge Subdivision utilizing most of the infrastructure already
in place.
As part of the original Meadow Creek Subdivision analysis, a Flood Study Report was prepared by
Allied Engineering Services, Inc. in 2005/2006. A copy of the report is included in Appendix A. The
City of Bozeman should have an approved copy of the report as well in their records. Stream 2 in
the Flood Study Report is the unnamed watercourse flowing within to the proposed Meadow
Bridge Subdivision. The post development hydrology in the Flood Study Report was calculated
using three separate methods, USGS Regression, SCS Curve Number, and Rational Method.
Ultimately, the Rational Method was selected as the hydrological calculation method. The
calculated post development 100-year flow for this stream was 41.42 cfs. Sanbell utilized the USGS
StreamStats application to compare the 100-year hydrology to the values calculated in the Flood
Study Report. StreamStats is a spatial analytical tool useful for water-resources planning and
management, and for engineering and design purposes. StreamStats calculated a 100-year flow of
38.1 cfs. Therefore, the 100-year flow in the Flood Study Report is realistic and appears to be
conservative. See Appendix B for the StreamStats Report.
The Flood Study Report demonstrates all the proposed culverts will convey the 100-year flow
MEMORANDUM PAGE 1 OF 2 MARCH 2O25
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without overtopping of roadways, and without exceeding the maximum headwater depth allowed
by the City of Bozeman of 1.5 times the diameter of the pipe. There are three (3) exiting 36-inch
equivalent arch reinforced concrete pipes within the proposed Meadow Bridge Subdivision
crossing Blackwood Road, Kurk Drive (identified as Ainsworth Drive in the record drawings), and
Parkway Avenue. In addition to the analysis provided in the Flood Study Report, Sanbell completed
an independent hydraulic capacity calculation of the culvert crossings utilizing FHWA HY-8
software. The HY-8 analysis was based on the record drawings of three (3) existing culvert
crossings and our results confirm the conclusions in the Flood Study Report. See Appendix C for
the record drawings of the culvert crossings and HY-8 output.
Based on the existing Flood Study Report prepared by Allied Engineering Services, Inc. and the
additional analysis prepared by Sanbell and presented in this Memorandum, we are requesting a
waiver of BMC 38.600.150.B. requiring another flood study be prepared for the Meadow Bridge
Subdivision Preliminary Plat. The existing Flood Study Report and additional analysis provide
sufficient information to determine flood risk within the proposed subdivision and demonstrate
that flood risk is sufficiently mitigated by the existing infrastructure.
APPENDICES
APPENDIX A - FLOOD STUDY REPORT - ALLIED ENGINEERING
APPENDIX B - STREAMSTATS REPORT
APPENDIX C - CULVERT CROSSING RECORD DRAWINGS & HY-8 RESULTS
MEMORANDUM PAGE 2 OF 2 MARCH 2O25
MEADOW BRIDGE SUBDIVISION
Project #BOZ-05021.28
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FLOOD STUDY REPORT
For Prelirr�inary Plat
Bozeman, Montana
Project: 04-170.2
August 30, 2005
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copy _ ot _ ALLIED
ENGINEERING
RERVICES, INC
32 Discovery Drive . Bozeman Montana 59718 . Ph: . Fax:
TABLE OF CONTENTS
Flood Shidy Report
- Introduction
- Description of Shidy Area
- Field Wark
- Hydrologic Analysis
- Hydraulic Analysis
- Results and Recommendations
- Figure 1 — Floodplain Basin Areas
- Figure 2 — Flood Study Area Plan (Overall)
- Figure 3 — Flood Shidy Area Plan
- Figure 4 — Flood Study Area Plan
- Figure 5 — Flood Study Area Plan
Appendix A — Hydrologic Analysis
Appendix B — Hydraulic Analysis
Appendix C — Background Infornlation
MEADOW CREEK SUBDNISION
FLOOD STUDY REPORT
Introduction
This report presents tl�e results of the preliminary flood study perfonned in conjunction with the
Meadow Creek Subdivision Preliminary Plat Application. The study has been performed to meet
Uie requirements of the City of Bozeman 2004 Unified Development Ordinance, section
18.58.090.
The flood study was performed to identify and quantify the flooding potential of the 4 small
creeks that traverse U1e subdivision. In several aspects of tl�e study, conservative assumptions
and u�ethods were employed to limit the scope and cost of the study. The results of the study
represent a conservative and safe approximation of the extents of possible flooding wiUiin the
subdivision, and provide critical infonnation for the further design of the subdivision layout and
associated improvements. As the details of the design of the subdivision and related
improvements are resolved, the flood study will be revisited and updated to allow the design of
the inost efficient and appropriate improvements.
The proposed subdivision is located directly west of South 19`h Avenue, approYimately '/ mile
south of Stucky Road. The site is located in partions of section 23, Township 2 South, Range 5
East, P.M.M. The USGS quad map shows two streams flowing from south to north and
converging near the northern end of the subdivision. This is generally correct, however upon
investigation of the site and review of other maps it was fotmd that the USGS quad map is in
error in delineating the westem tributary. The west tributary as shown on the USGS map is
achially an irrigation canal owned by the Middle Creek Ditch Company. To avoid confiision, all
exhibits sliow the coirect locations of both the creek and the irrigation ditch. For the sake of the
study, the streams have been ]abeled as stream 1 for the westem tributary, stream 2 for the
eastem tributary, and stream 3 for the stream formed by the merging of streams 1 and 2.
According to the NRCS, these streams are un-named triUutaries of East Baxter Creek. A fourth
small stream, E. Catron Creek, also flows through the subdivisiou from north to south near the
eastern boundary. This stream will be referred to as stream 4 in this report. Streams 1 through 4
have drai»age basin areas of 143, 126, 307, and 105 acres, respectively. The Gallatin
Conseivation Dishict 310 jurisdiction map shows the streams as perennial streams. Figure 1
shows the drainage basins and stream locations.
As the total drainage area is less than 25 sqtiare miles, the floodplain submission for the
preliminary plat falls under the requirements of subsection B.2 of the City of Bozeman 2004
Unified Development Ordinance, section 18.58.090. This section does not explicitiy require a
full floodplain analysis report. This flood study will, however, meet all requirements of the
floodplain analysis report other than providing a detailed floodplain boundary map.
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Description of Study Area
The creeks within the subdivision ariginate roughly a mile souTh of the subdivision and receive
flow from precipitation runoff and �roundwater. As the groundwater in thc area is known to be
sl�allow, it is likely that virtually all of the flow in the creeks is from groundwater contributions
during the drier months of the year.
Tl�e drainage basin areas within the subdivision are grass pasture land with some shrubbery,
trees, and wetlands near the creeks themselves. The areas of the draina�e bt�sins upstream to the
south of the subdivision are generally irrigated farniland; well covered, maintained and mowed
for hay. Essentially all of the drainage basin areas are currently undeveloped.
The streams themsetves are for the most part fiee-flowing and currently unrestricted. The
northern stream, streatll 3, has one or two existing CMP culverts at driveway locations for the
northern house and farm outUuildings. These culverts will be removed during the construction of
the subdivision improvements. Another CMP culvert can be found under the driveway of the
residence in the southeastern area of the subdivision on streun 4. It appears tlte area upstrean� of
the end of tl�e culvert experiences some flooding due to the culvert constricting the floodplain, so
some work may need to be done to redtice Yhis flooding. The flooding is likely contained by the
area tllat will be dedicated as park, buC we recoimnend eliininating this culvert as part of the park
plan.
An onsite walkthrougll of the streams was conducted in June of tl�is year. The walkthrougl�
showed that the three major streams, while not very deep, had very broad channels with the
apparent capability to contain the flood waters. At the junction of streams I and 2 there is
currently a man-made dam that forms a small pond. A small spillway at the northeast corner of
the pond propagates the stream flow to the north. The pond will remain virtually tmchanged
after the development of the subdivision, but the spillway will need to be improved to safely
convey the potenYial flows and prevent overtopping of the dam. The Middle Creek irrigation
ditch flows into the stream immediately below the dam and pond. Stream 3, downstream of the
pond, flows throug}� an area that is cutrently used for grazing cattle. TUe stream becomes
basically a perched ditch through this area, where the land to the west of the stream is lower in
elevation thau the stream. The sh�eam continues to the north where it hirns east near the
subdivision boundary and heads into the Genesis Business Park. A man-made channel nms
around the southwest corner of tlie Genesis Business Park, just west of the where the stream
turns east The channel is constricted by fill placed for the building at the end of Enterprise
Boulevard in Genesis Business Park. This chaimel currently drains the low area near the perclied
section of the streani, and also receives any flow that overtops ihe small chamiel of the perdied
stream. The man-made channel daylights into a vacuit field to the north of the subdivision and
west of Genesis Park. As the man-made channel will certainly see a significant portion of the
flood waters and is constricted, the conservative decision was made to Uegin the flood study with
the downstream end being the man-made channel.
The entire length of stream 4 was examined on the site. Special attention was given to the
locations of proposed driveway and street crossings, where culverts will be placed. The channel
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of stream 4 was found to be £airly wide compared to the width of the flow of water. The channel
widths were found to be about 15 to 25 feet, and the flow of water in the channel at the time was
fi'om 2 to 3 feet in width. Beyond tl�e channel, the grotmd slopes up contimiously away from the
stream for the entire len�th of the stream witltin the subdivisiou. Because the park and wetland
setback boundaries for tl�is streain are over 100 feet wide, and tlie topo�raphy and nature of the
stream do not appear to be conducive to flooding, it was decided that a detailed survey and
floodplain analysis would not be performed for stream 4. Culverts for the road crossing will be
sized individually so that any headwater at the upstream eud will not encroach beyond tl�e
boundaries of the wetland setback and parks.
The walkthrough allowed several key elements of tl�e flood shidy to be identified a��d
recogilized. Items noted included: ground cover and vegetation, topographic features, aud
stream characteristics. No indications or signs of past flooding were observed.
Field Work
A topographic survey of the subject property was perfonned by Allied En�ineering in 1999 as
part of the preliminary stages of a subdivision proposaL The survey was done using survey
grade GPS equipment and conventional survey equipment. The survey done in 1999 did not
encompass the entire subdivision that is currently plamted for development, but did thoroughly
cover tl�e entire area of streams 1 through 3. The original survey was done based on a relative
coordinate system, and for this project was converted to a vertical datum of NAVD88 and a
horizontal datum of Montana State Plane Coordinates, NAD83 with imits of International Feet.
The survey data was used to create a digital terrain model, from which floodplain cross sections
could be sampled.
Afrer the engineers' site visit for the flood study, it was noriced that the southern end of stream 1,
in an area witl� heavy tree cover, had not been sufficiently surveyed in 1999 for a representative
digital terrain model to be created. In late June of 2005, 4 cross sections were surveyed at tlie
southem end of stream 1 to be used for the flood study in place of the dijital terrain model in this
area. At the same time 3 cross sections at the north end of the subdivision and the southwest
corner of Genesis Business Par]< were surveyed. The 3 northern cross sections, it was thought,
would allow the accurate modeling of the floodplain in the man-made channel, for whicl� no
survey data existed. Also the addition of one or two more cross sections iinmediately
downsh�eam of the study area may greatly increase the accuracy of the model at the very
downstream end of the creek, at the northern subdivision boundary.
A suivey of the channel of stream 4 was conducted in the spring of 2005 primarily to determine
the location and alignment of the stream. Because very limited survey data was obtained, iC was
wiclear if the survey data would be sufficient enough to perform a floodplain analysis of stream
4.
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HvdroloQic Anah�sis
Tite drainage basins which contribute runoff to each of the 4 streams in tlle subdivisions were
delineated using the 1999 sEirvey contours for the area within tlie subdivision, and tl�e USGS
topographic contours for tl�e areas to tl�e south of the subdivision and areas within the
subdivision not covered by the 1999 survey. Fi�ure 1 shows the draina�e basins and their areas.
It was decided that tUree methods for calculating the flood flows would be employed, and that
flows for both the pre-development and post-development condition would be calculated. The
flow to Ue used for the flood study and improvements design would then be selected from the
range of calculated values. The three �nethods used were: the Rational Metllod, SCS Curve
Number Method, and USGS Regional Regression Equations Uased on basin characteristics.
Return frequencies of 10, 25, and 100 years were used with each method. Pre and post
development flows were calculated for the rational and SCS methods, but the USGS re�ression
equations only apply to the pre-development condition. It should also be noted that the post-
development coefficients were applied to the entire drainage basin areas. This is another
conservative approximarion, in that the only portion of the drainage basins that will be developed
upon the completion of tl�e subdivision is the subdivision area itsel£ It was thought very likely
that the area of the drainage basins up-gradient of the subdivision would see deve}opment in the
firture.
The Rational Method is typically the most comi��only accepted method for smaller draivage
areas. It is also the method required by the City of Bozeman Design Standards and
Specifications to be used for the sizing of storm drainage facilities. The calculated flow rates are
directly proportional to the area, rainfall intensity, and a C factor that is mandated by the city for
pre and post development conditions. The C factor, in this case, is not dependant on regional
characteristics, soil types, vegetation qualities, or elevation.
The SCS Curve Number method is a less-frequenUy employed method for calculatin� runoff
flow rates. The appealing aspect of the SCS method is that the Curve Number variable used in
tUe calcttlation is selected based on several quantitative and qualitative parameters, such as
NRCS soil types, land uses, and vegetation.
A common parameter to both the rational method and the SCS curve number method is the time
of concentration. The time of concentration used for both methods was calculated using
Manning's Kinematic Sol�ttion for the overland flow, and then Manning's formula for open
channel hydraulics for the flow in the channels. The velocity of the water in the channel was
calculated assuming that the channel was full. For flows and areas of the stream where the
channel is actually not flowing full, this assumption will yield a smaller time of concenh�ation.
The assumpYion is conseivative in this case, and was made to eliminate the need to iterate several
times back and forth in order to exactly calculate the time of concentration.
The third method utilized in calctilatin� the flood flow was the USGS Regional Regression
Equations. The equations are provided by the USGS publication "Methods for Estimating Flood
Frequency in Montana Based on Data through Water Year 1998", for the Upper Yellowstone —
Central Mountain region. The USGS regression equations are specific to the area for which they
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represent, and are largely dependant on the elevation of the shidy area. Tl�e equatious are
empirical in nahire, and are assembled from actual data recorded fi-oin stream ga�es and other
sotirces.
The results of tlle hydrologic analysis for all 4 drainage basins can be found in Appendix A of
this report. As was expected, the flood flows vaiied between methods and pre and post
development Tl�e flow values setected for use in the flood study for all 4 basins were the
Rational Method post-development flows. The USGS Regression values were not selected
because the flows varied greatly and inconsistently fi-om the values calculated witli tlie otlier
methods. The regression equations, it is known, generally are mare accurate for basins of a
much larger size, on the order of several square miles. The SCS Curve Number Method values
were uot selected due to the fact that the nature of the soils of the area indicated a curve number
to use in the calculation that yielded quite small pre-development flow values. By process of
elimination, the rational method values were selected for use with the floodplain shidy. 'I'he
post-development flow values were selected as development is very likely to occur in the future.
FurtUermore, while new subdivisions are required to limit runoff from the developed area to pre-
development levels by use of detention ponds, the ponds are typically only sized for a 10-year
event.
It was decided to include a quantity of tlow to drainage basin 3 to accowit for the potential flow
contribution of tUe Middle Creek ditch fork that en4ers the stream just downstream from the pond
and the jwiction of streains 1 and 2. A site inspection of the ditch upstream of the subdivision
revealed U�at the fork of the ditch that traverses the subdivision lies on a slight topographic ridge
with little if any poYential for intercepting runof£ The main Middle Creek ditch, however, does
have the potential to intercept a significant amount of nmoff. It was decided that the ditch that
contributes flow to drainage basin 3 would be evaluated, and that the maximum possible flow
that tl�e ditch could convey would be used. This assumption is a conservative one, but withotit
spending a great deal of time analyzing the Middle Creek ditch system the flow could not
otherwise be determined. Hydraulic calculations were perfornled to evaluate the headgate that
allows flow into the ditch about 1.5 miles soutli of the subdivision and the nearby secYions of the
ditcli itsel£ It was concluded that 13.5 cfs could potentially flow throu;h the headgate and ditch,
and so this flow value was added to the hydrologic flow values for draina�e basin 3 to be used in
the floodplain analysis. The hydraulic calculations and details of the ditch can be found in
Appendix C of this report. The 100-year flows used in the flood study are sutnmarized below:
Basin 1 Basin 2 Basin 3 Basin 4
Post-Development Rational 44.22 cfs 41.A2 cfs 92.65 cfs 28.18 cfs
Method 100-Yr Flow
Hvdraulic Analvsis
Floodplain modeling was performed using the U.S. Army Corp of Engineers Hydrologic
Engineering Center — River Analysis System (HEC-RAS) computer program version 31.1
(Army Corps of En�iiteers, 2003). The computer program Are-View 3.2 with extensions 3D
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Analyst (ESRI, 1999) and HEC-GeoRAS (Anny Corps of Engineers, 2002) was used to create a
georeferenced ivput gcometry file for HEC-RAS.
Initial Mannine's n values for the chamlel and overbanks were estimated fro�n a combination of
reference documents and experience from past floodplain projects. The first computation run of
HEGRAS showed several cross-sections going to supercritical flow. Because the strea�ns do not
l�ave the slope or physical characteristics of a stream that perpetuates supercritical flow, the
supercritical results indicated that the Manning's n values used were too low. The Ma�tning's n
values were increased sli�htly, the computations were run again, and the results were much more
realistia The Manning's n values arrived at were 0.06 for tl�e chaimels, and 0.065 for tlie
overbanks.
The stream geometry created for the analysis was based on the existing streams, and additions
were made to reflect the plans for the subdivision improvements. Cross sections for tlie
hydraulic uialysis were spaced along tl�e streams at a distance of approximately 300 feet, with
additional cross sections being located at changes in alignment and profile. The HEC-RAS
"interpolated XS's" routine was used to provide supplemental XS's where necessary. Culverts
were placed at all of the proposed road crossings for the subdivision streets. Bridges may be
constructed for some of the streani crossings but at Hlis time no concrete plans have been made,
so for the sake of the floodplain analysis culverts were incorporated to present a worst-case
scenario. Initial culvert sizes were input, and after various calculation nms were made, the sizes
were adjusted to refine headwater depths and flood water levels for the 100-year flows. All of
the proposed culverts will flow the 100-year flood flow with no overtopping of roadways, and
without exceeding the maximum headwater depth allowed by the City of Bozeman of 1.5 times
the dia�neter of the pipe. Tl�e culverts were modeled as arch reinforced concrete pipe. The
flatter channels of the arch pipe are more desirable to permitting agencies, and the shorter height
of the arch section redtices fill quantities. The inverts of Uie culverts were also placed 0.5 feet
below the natural channel bottom, which is a newer require�nent of the sh�eain permitting
agencies. The headwater depths of the flood water at the culverts of the subdivision are
siunmarized in the following table:
Culvert Size Headwater Depth (ft)
Stream 1 Cu1v. 1 42" Equiv. Arcli RCP 2.04
Stream 3 Culv. I 48"Equiv. Arch RCP 3.51
Stream 3 Culv. 2 36" Equiv. Arch RCP 2.17
Stream 2 Culv. 1 36" Equiv. Arch RCP 2.29
Stream 2 Culv. 2 36"Equiv. Arch RCP 2.47
Results and Recommendations
HEGRAS output results can be found in Appendix B of this report. The results basically
confinned the engineers' initial in2pressions of the stream, in that the flood would mostly be
contained within the channels of the streams. A few of the lots on the west side of stream 1 near
the upper end of the reach may experience some very shallow flooding. While this is not a
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Preliminary Flood Study Report Project:04-170.Y Meadow Creelc Subdivision
AuRust 30,4006
FEMA recognized floodplain stream, and the development and constniction on these lots will not
be governed by the usual floodplain development requirements, we recommend that certain
requirements be met regardless. We recommend that the construction of homes on these lots
meet the requirements of the City of Bozeman Unified Development Ordinance Floodplain
Regulations, specifically the following: "The new consriuction, alterations and substantial
improvements of residential shuctures including manufachued homes must be consiructed on
suitable fill such that the lowest floor elevation (includin�basement) is 2 feet or more above the
base flood elevation. The suitable fill shall be at an elevation no lower than the base flood
elevation and shall extend for at least 15 feet, at that elevation, beyond the structure(s) in all
directions."
Figures 2, 3, 4, and 5 show the details of the floodplain analysis, proposed lot and street layout,
and recommended improvements with respect to the stream floodplains.
Allied Engineering Services,Inc.
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Benj in J. Cope, EI Paul J. Sanford, PE
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REFERENCES
Anny Coips of Engineers, (2003). "Rive�- Analysis System — HEGIL9S", version 3.11, Davis,
California.
Army Corps ofEngineers, (2002). "HEC-GeoRAS", version 3.L1, Davis, Califoinia.
Enviromnental Systems Research Institute (ESRI), Inc., (1999). "ArcView GIS 3.2".
FEMA, (1984). "Tlood Insimance Study: Gallatin County, A�Iontana".
Haestad Methods, (2003). "Culver�t Master", version 2.0. Waterbury, CT.
NRCS, (1996). "Soil Sau•vey of Gallatin Counry Area, Montana".
USGS, (2004). "Methods for Estinzating Flood Freclue�rcy in Montana Basecl on Data through
W¢ter Year 1998", U.S. Geological Survey.
Allied Engineering Se�vices, Inc. Page 8
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Middle Creek StreamStats Report
Region ID: MT
WorkspacelD: MT20250204172337277000
Clicked Point(Latitude, Longitude): 45.64225,-111.06890
NHD Stream GNIS Name of Click Point:A Middle Creek Ditch
Time: 2025-02-04 1 0:24:09 -0700
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� Basin Characteristics
Parameter Code Parameter Description Value Unit
CHANWD_RS Channel width determined from remotely sensed data sources, including aerial imagery 0 feet
CONTDA Area that contributes flow to a point on a stream 0.1 square miles
DRNAREA Area that drains to a point on a stream 0.1 square miles
EL6000 Percent of area above 6000 ft 0 percent
WACTCH Width of active channel 0 feet
WBANKFULL Width of channel at bankfull 0 feet
� Peak-Flow Statistics
Peak-Flow Statistics Parameters [UpYellow CentMount Region BasinC 2015 5019F]
Parameter Code Parameter Name Value Units Min Limit Max Limit
CONTDA Contributing Drainage Area 0.1 square miles 0.39 2040
EL6000 Percent above 6000 ft 0 percent 0 100
Peak-Flow Statistics Parameters [UpYllw CentMount Region Act Channel SIR 2020 5142]
Parameter Code Parameter Name Value Units Min Limit Max Limit
WACTCH Width Of Active Channel 0 feet 1 150
Peak-Flow Statistics Parameters [UpYllw CentMount Region Bankfull SIR 2020 5142]
Parameter Code Parameter Name Value Units Min Limit Max Limit
WBANKFULL Width Of Bankfull Channel 0 feet 2.5 170
Peak-Flow Statistics Parameters [UpYllw CentMount Region Aerial Photo SIR 2020 5142]
Parameter Code Parameter Name Value Units Min Limit Max Limit
CHANWD_RS Channel_Width_remotely_sensed 0 feet 2.3 191.9
Peak-Flow Statistics Disclaimers [UpYellow CentMount Region BasinC 2015 5019F]
One or more of the parameters is outside the suggested range. Estimates were extrapolated with unknown errors.
Peak-Flow Statistics Flow Report [UpYellow CentMount Region BasinC 2015 5019F]
Statistic Value Unit
66.7-percent AEP flood 0.411 ft^3/s
50-percent AEP flood 0.746 ft^3/s
42.9-percent AEP flood 1.03 ft^3/s
20-percent AEP flood 3.47 ft^3/s
10-percent AEP flood 7.46 ft^3/s
4-percent AEP flood 1 6 ft^3/s
2-percent AEP flood 25.7 ft^3/s
1-percent AEP flood 38.1 ft^3/s
0.5-percent AEP flood 54.4 ft^3/s
0.2-percent AEP flood 82.5 ft^3/s
Peak-Flow Statistics Disclaimers [UpYllw CentMount Region Act Channel SIR 2020 5142]
One or more of the parameters is outside the suggested range. Estimates were extrapolated with unknown errors.
Peak-Flow Statistics Flow Report [UpYllw CentMount Region Act Channel SIR 2020 5142]
Statistic Value Unit
Active chan width 66.7 percent AEP flood 0 ft^3/s
Active Channel Width 50-percent AEP flood 0 ft^3/s
Active chan width 42.9 percent AEP flood 0 ft^3/s
Active Channel Width 20-percent AEP flood 0 ft^3/s
Active Channel Width 10-percent AEP flood 0 ft^3/s
Active Channel Width 4-percent AEP flood 0 ft^3/s
Active Channel Width 2-percent AEP flood 0 ft^3/s
Active Channel Width 1-percent AEP flood 0 ft^3/s
Active Channel Width 0.5-percent AEP flood 0 ft^3/s
Active Channel Width 0.2-percent AEP flood 0 ft^3/s
Peak-Flow Statistics Disclaimers [UpYllw CentMount Region Bankfull SIR 2020 5142]
One or more of the parameters is outside the suggested range.Estimates were extrapolated with unknown errors.
Peak-Flow Statistics Flow Report [UpYllw CentMount Region Bankfull SIR 2020 5142]
Statistic Value Unit
Bankfull width 66.7 percent AEP flood 0 ft^3/s
Bankfull Width 50-percent AEP flood 0 ft^3/s
Bankfull width 42.9 percent AEP flood 0 ft^3/s
Bankfull Width 20-percent AEP flood 0 ft^3/s
Bankfull Width 10-percent AEP flood 0 ft^3/s
Bankfull Width 4-percent AEP flood 0 ft^3/s
Bankfull Width 2-percent AEP flood 0 ft^3/s
Bankfull Width 1-percent AEP flood 0 ft^3/s
Bankfull Width 0.5-percent AEP flood 0 ft^3/s
Bankfull Width 0.2-percent AEP flood 0 ft^3/s
Peak-Flow Statistics Disclaimers [UpYllw CentMount Region Aerial Photo SIR 2020 5142]
One or more of the parameters is outside the suggested range.Estimates were extrapolated with unknown errors.
Peak-Flow Statistics Flow Report [UpYllw CentMount Region Aerial Photo SIR 2020 5142]
Statistic Value Unit
Rem sens chan width 66.7 percent AEP fld 0 ft^3/s
Rem_sens_chan_width_50_percent_AEP_flood 0 ft^3/s
Rem sens chan width 42.9 percent AEP fld 0 ft^3/s
Rem_sens_chan_width_20_percent_AEP_flood 0 ft^3/s
Rem_sens_chan_width_10_percent_AEP_flood 0 ft^3/s
Rem_sens_chan_width_4_percent_AEP_flood 0 ft^3/s
Rem_sens_chan_width_2_percent_AEP_flood 0 ft^3/s
Rem_sens_chan_width_1_percent_AEP_flood 0 ft^3/s
Rem_sens_chan_width_0_5_pct_AEP_flood 0 ft^3/s
Rem_sens_chan_width_0_2_pct_AEP_flood 0 ft^3/s
Peak-Flow Statistics Flow Report [Area-Averaged]
Statistic Value Unit
66.7-percent AEP flood 0.411 ft^3/s
50-percent AEP flood 0.746 ft^3/s
42.9-percent AEP flood 1.03 ft^3/s
20-percent AEP flood 3.47 ft^3/s
10-percent AEP flood 7.46 ft^3/s
4-percent AEP flood 16 ft^3/s
2-percent AEP flood 25.7 ft^3/s
1-percent AEP flood 38.1 ft^3/s
0.5-percent AEP flood 54.4 ft^3/s
0.2-percent AEP flood 82.5 ft^3/s
Active chan width 66.7 percent AEP flood 0 ft^3/s
Active Channel Width 50-percent AEP flood 0 ft^3/s
Statistic Value Unit
Active chan width 42.9 percent AEP flood 0 ft^3/s
Active Channel Width 20-percent AEP flood 0 ft^3/s
Active Channel Width 10-percent AEP flood 0 ft^3/s
Active Channel Width 4-percent AEP flood 0 ft^3/s
Active Channel Width 2-percent AEP flood 0 ft^3/s
Active Channel Width 1-percent AEP flood 0 ft^3/s
Active Channel Width 0.5-percent AEP flood 0 ft^3/s
Active Channel Width 0.2-percent AEP flood 0 ft^3/s
Bankfull width 66.7 percent AEP flood 0 ft^3/s
Bankfull Width 50-percent AEP flood 0 ft^3/s
Bankfull width 42.9 percent AEP flood 0 ft^3/s
Bankfull Width 20-percent AEP flood 0 ft^3/s
Bankfull Width 10-percent AEP flood 0 ft^3/s
Bankfull Width 4-percent AEP flood 0 ft^3/s
Bankfull Width 2-percent AEP flood 0 ft^3/s
Bankfull Width 1-percent AEP flood 0 ft^3/s
Bankfull Width 0.5-percent AEP flood 0 ft^3/s
Bankfull Width 0.2-percent AEP flood 0 ft^3/s
Rem sens chan width 66.7 percent AEP fld 0 ft^3/s
Rem_sens_chan_width_50_percent_AEP_flood 0 ft^3/s
Rem sens chan width 42.9 percent AEP fld 0 ft^3/s
Rem_sens_chan_width_20_percent_AEP_flood 0 ft^3/s
Rem_sens_chan_width_10_percent_AEP_flood 0 ft^3/s
Rem_sens_chan_width_4_percent_AEP_flood 0 ft^3/s
Rem_sens_chan_width_2_percent_AEP_flood 0 ft^3/s
Rem_sens_chan_width_1_percent_AEP_flood 0 ft^3/s
Rem_sens_chan_width_0_5_pct_AEP_flood 0 ft^3/s
Rem_sens_chan_width_0_2_pct_AEP_flood 0 ft^3/s
Peak-Flow Statistics Citations
Sando, Roy, Sando, S.K., McCarthy, P.M., and Dutton, D.M.,2016, Methods for estimating peak-flow frequencies at ungaged sites in
Montana based on data through water year 2011: U.S. Geological Survey Scientific Investigations Report 2015-5019—F,30 p.
(https://doi.org/10.3133/sir20155019)
Chase, K.J., Sando, R.,Armstrong, D.W., and McCarthy, P.,2021, Regional regression equations based on channel-width
characteristics to estimate peak-flow frequencies at ungaged sites in Montana using peak-flow frequency data through water year
2011 (ver. 1.1, September 2021): U.S. Geological Survey Scientific Investigations Report 2020-5142, 49 p.
(https://doi.org/10.3133/sir20205142)
� NHD Features of Delineated Basin
NHD Streams Intersecting Basin Delineation Boundary
This functionality attempts to find the stream name at the delineation point.The name of the nearest intersecting National Hydrography Dataset(NHD)
stream is selected by default to appear in the report above. NHD streams do not correspond to the StreamStats stream grid and may not be accurate. If
you would like a different stream to appear in the above section,please make a selection below.
GNIS ID GNIS Name Distance from Clicked Point(ft) Feature Type Selected Stream Name
00787233 Middle Creek Ditch 3,191.31 Canal Ditch � Middle Creek Ditch
Watershed Boundary Dataset(WBD)HUC 8 Intersecting Basin Delineation Boundary
This functionality attempts to find the intersecting HUC 8 of the delineated watershed. HUC boundaries do not correspond to the StreamStats data and
may not be accurate.
HUC 8 Name
10020008 Gallatin
NHD Hydro%gic Features Citations
U.S. Geological Survey, 2022, USGS TNM - National Hydrography Dataset,accessed July 21,2022 at URL
https://hydro.nationalmap.gov/arcgis/rest/services/nhd/MapServer/6.
(https://hydro.nationalmap.gov/arcgis/rest/services/nhd/MapServer/6) U.S. Geological Survey, 2022, USGS TNM - National
Hydrography Dataset, accessed July 21, 2022 at URL https://hydro.nationalmap.gov/arcgis/rest/services/wbd/MapServer/4.
(https://hydro.nationalmap.gov/arcgis/rest/services/wbd/MapServer/4)
� Channel-width Methods Weighting
No method weighting results returned.
USGS Data Disclaimer:Unfess otherwise stated,all data,metadata and related materials are considered to satisfy the quality standards relative to the purpose forwhich
the data were collected.Although these data and associated metadata have been reviewed for accuracy and completeness and approved for release by the U.S.Geological
Survey(U5G5),no warranty expressed or implied is made regarding the display or utility of the data for other purposes,nor on all computer systems,nor shall the act of
distribution constitute any such warranty.
USGS Software Disclaimer:This software has been approved for release by the U.S.Geological Survey(USGS).Although the software has been subjected to rigorous review,
the USGS reserves the right to update the software as needed pursuant to further analysis and review.No warranty,expressed or implied,is made by the USGS or the U.S.
Government as to the functionality of the software and related material nor shall the fact of release constitute any such warranty.Furthermore,the software is released on
condition that neither the USGS nor the U.S.Government shall be held liable for any damages resulting from its authorized or unauthorized use.
USGS Product Names Disclaimer:Any use of trade,firm,or product names is for descriptive purposes only and does not imply endorsement by the U.S.Government.
Application Version:4.26.0
StreamStats Services Version:1.2.22
NSS Services Version:2.2.1
MEADOW BRIDGE SUBDIVISION
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NOTE�
-EXISTING UNDERGROUND INSTALLATIONS 8c PRIVATE UTILJl1E5 SH01h�N ARE INDICATED ACCORDING TO THE BEST INFORMAl10N AVAILABLE TO � � �
THE ENGINEER. THE ENGINEER DOES NOT GUARANTEE THE ACCURACY OF SUCH INFORMATION, SERVICE LINES (WATER, POWER, GAS, STORM, �
5E'NER, TELEPHONE & TELEVI510N) MAY NOT BE STRAIGHT LJNES OR AS INDICATED ON THE PLANS, STATE LAW REQUIRES CONTRACTOR TO V V
CALL ALL Ul1LJTY COMPANIES BEFORE EXCAVATION FOR EXACT LOCATIONS, y�
-ALL IMPROVEMENTS SHALL BE PERFORMED IN ACCORDANCE 1hfITH k10NTANA PUBLIC WORKS STANDARD SPECIFICATIONS 5TH EDITION, MARCH,
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2003, AND THE CITY OF BOZEMAN STANDARD MODIFICATIONS, DATED MARCH, 2004 AND ADDENDUM No. 1. �
-UNLE55 OTHERWISE SPECIFIED, ALL CONSTRUCTI�N LAYOUT AND STAKING SHALL BE PERF�RMED UNDER THE RESPONSIBLE CHARGE OF A
LAND SURVEYOR LICENSED IN THE STATE OF MONTANA AND BY A PARTY CHIEF OR ENGINEERING TECHNICIAN EXPERIENCED IN CONSTRUCl10N
LAYOUT AND STAKING TECHNI4IJES AS ARE REQIJIRED BY THE SPECIFIC TYPE aF UJORK BEING PERFORA�ED_
-BENCHMARK �1; SECTI�M C�RMER (REBAR) COMMON TO 5EC110N5 23, 24, 25 & 26
E 50303�75 HATCHED AREA WITHIN STREET DENOTES SURFACE IMPROVEMENTS, `,�10�� T yf��i���If
E L E V, = 5 0 2 3.2 8 IF NO HATCHING IS SHOWN, SURFACE IMPROVE�AENTS 4�1ERE NOT t�� � � �
COIr1PLETED UNDER THIS CONTRACT. ti�r ��
-BENCHMARK �2: WITNE55 CORNER ("MMCSSA�� YELL01hf CAPPED REBAR) TO SECTION CORNER COMMON TO SECTIONS 13, 14, 23 & 24 � r KURT W. �
N 40219.41 SCALE �� THOMSON ��
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-SUBTRACT 19,45 FEET FROM BENCHMARK #1 OR �2 ELEVATI�N T� CONVERT TO COB DATUM. VERT. : 1 " = 5' U TI LI TI ES — a�TaB ER� �V V�
-ANY EXISIING OR NEW VALVES WHICH CONTROL THE COB�s WATER SUPPLY SHALL BE 4PERATED BY COB PERSONNEL ONLY. �T R E E T S — N a V E M B E R� �V V�
- THE CaNTRACTOR SHALL NOl1FY THE 1iVATER DEPARTMENT A MINIMUM OF 24-HOURS PRI�R TO BEGINNING ANY WORK,
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NOTE�
-EXISTING UNDERGROUND INSTALLAl10NS & PRIVATE UTILJl1E5 SH01h�N ARE INDICATED ACCORDING TO THE BEST INFORMAl10N AVAILABLE TO �
THE ENGINEER. THE ENGINEER DOES NOT GUARANTEE THE ACCURACY OF SUCH INFORMATION, SERVICE LINES (WATER, POWER, GAS, STORM, � ����y��1 T �f���i�
5E'NER, TELEPHONE & TELEVI510N) MAY NOT BE STRAIGHT LJNES OR A5 INDICATED ON THE PLANS, STATE LAW REQUIRES CONTRACTOR TO � t��� �°' � ��y
CALL ALL Ul1LJTY COMPANIES BEFQRE EXCAVATION FOR EXACT LOCATIONS, ti�= �_
-ALL IMPROVEMENTS SHALL BE PERFORMED IN ACCORDANCE 1hfITH k10NTANA PUBLIC WORKS STANDARD SPECIFICATIONS 5TH EDITION, MARCH, » » �� r THOMSON �;
2003, AND THE CITY OF BOZEMAN STANDARD MODIFICATIONS, DATED MARCH, 2004 AND ADDENDUM No. ,. � R — � E N �TE S A S — B U �T C � N D T �N
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-UNLE55 OTHERWISE SPECIF1ED, ALL CONSTRUCTI�N LAYOUT AND STAKING SHALL BE PERF�RMED UNDER THE RESPONSIBLE CHARGE OF A �fi Cr�y�� -?�
LAND SURVEYOR LICENSED IN THE STATE OF MONTANA AND BY A PARTY CHIEF OR ENGINEERING TECHNICIAN EXPERIENCED IN CONSTRUCl10N i/!�� �i�S��4h���C7��1
LAYOUT AND STAKING TECHNIQUES AS ARE REQUIRED BY THE SPECIFIC TYPE OF 1NORK BEING PERFORA�ED_ � ��ri�QNAL �������
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N 34897,73 HATCHED AREA YVITHIN STREET DENOTES SURFACE IMPROVEk1ENTS. SCALE
E 50303,75 IF NO HATCHING IS SHOtikN, SURFACE IMPROYEMENTS WERE NOT
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ELEV, = 4939.18 VERT. : 1 " = 5�
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-ANY EXISTING OR NEW VALVES WHICH CONTR�L THE COB�s WATER SUPPLY SHALL BE OPERATED BY COB PERSONNEL ONLY.
- THE CaNTRACTOR SHALL NOl1FY THE �1ATER DEPART�IENT A MINI�IUM OF 24-HOURS PRIOR TO BEGINNING ANY WORK.
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HY-8 Culvert Analysis Report
Crossing Discharge Data
Discharge Selection Method: Specify Minimum, Design,and Maximum Flow
Minimum Flow: 7.46 cfs
Design Flow: 16.00 cfs
Maximum Flow: 41.42 cfs
Table 1-Summary of Culvert Flows at Crossing: Blackwood RD
Headwater Total Culvert 1 Roadway Iterations
Elevation (ft) Discharge Discharge Discharge
(cfs) (cfs) (cfs)
17.93 7.46 7.46 0.00 1
18.14 10.86 10.86 0.00 1
18.36 14.25 14.25 0.00 1
18.47 16.00 16.00 0.00 1
18.79 i 21.04 i 21.04 i 0.00 i 1 �
19.02 24.44 24.44 0.00 1
19.25 � 27.84 � 27.84 � 0.00 � 1 �
19.49 31.23 31.23 0.00 1
19.74 34.63 34.63 0.00 1
20.00 38.02 38.02 0.00 1
20.28 41.42 41.42 0.00 1
22.00 58.91 58.91 0.00 Overtopping
Rating Curve Plot for Crossing: Blackwood RD
Total Ratui�Cuive
Crossina Black-���ood RD
220
21.5
21.0
c 20_5
0
� -
� -
a�
W 20_0
a� -
m
3 -
� 19_5
a, -
S -
19A
18.5
18_0
5 10 15 20 25 30 35 40 45 50 55 60 65
Total Discharge(cfs)
Culvert Data: Culvert 1
Table 1-Culvert Summary Table: Culvert 1
Total Culve Head Inle Outl Fl Nor Criti Out Tailw Outl Tailw
Disch rt water t et ow mal cal let ater et ater
arge Disch Elevat Cont Cont Ty Dep Dep De Dept Velo Veloc
(cfs) arge ion rol rol pe th th pth h (ft) city ity
(cfs) (ft) Dep Dep (ft) (ft) (ft) (ft/s (ft/s)
th th )
(ft) (tt)
7.46 7.46 17.93 0.87 0.0* 1- 0.42 0.63 1.0 1.06 2.21 2.38
cfs cfs JS1 6
t
10.86 10.86 18.14 1.08 0.0* 1- 0.51 0.77 0.5 1.15 7.74 2.40
cfs cfs S2 1
n
14.25 14.25 18.36 1.30 0.0* 1- 0.58 0.90 0.5 1.21 8.49 2.49
cfs cfs S2 8
n
16.00 16.00 18.47 1.41 0.0* 1- 0.62 0.96 0.6 1.24 8.65 2.54
cfs cfs S2 3
n
21.04 21.04 18.79 1.73 0.0* 1- 0.72 1.12 0.7 1.30 9.43 2.67
cfs cfs S2 4
n
24.44 24.44 19.02 1.96 0.0* 1- 0.79 1.22 0.8 1.34 9.69 2.75
cfs cfs S2 2
n
27.84 27.84 19.25 2.19 0.20 1- 0.85 1.32 0.8 1.37 10.5 2.83
cfs cfs 0 S2 5 5
n
31.23 31.23 19.49 2.43 0.43 5- 0.91 1.41 0.9 1.40 10.4 2.90
cfs cfs 0 S2 5 4
n
34.63 34.63 19.74 2.68 0.72 5- 0.97 1.49 1.0 1.43 10.8 2.96
cfs cfs 6 S2 1 1
n
38.02 38.02 20.00 2.94 1.03 5- 1.03 1.57 1.0 1.45 11.0 3.02
cfs cfs 9 S2 7 8
n
41.42 41.42 20.28 3.22 1.36 5- 1.09 1.65 1.1 1.48 11.3 3.08
cfs cfs 8 S2 4 0
n
*Full Flow Headwater elevation is below inlet invert.
Culvert Barrel Data
Culvert Barrel Type Straight Culvert
Inlet Elevation (invert): 17.06 ft,
Outlet Elevation (invert): 15.16 ft
Culvert Length: 108.02 ft,
Culvert Slope: 0.0176
Culvert Performance Curve Plot: Culvert 1
PerfoiYuance Curve
c,��� c,�n��c i
� 0
Inlet Control Elev Outlet Control Elev
220
21.5
21_0
20_5 -�
c 20 O .
o -
� 19_5
a, -
W
a� �g� _ i"
� - �
� 18_5 .�
a�
= 18A -�
_ �_
1Z5 �"�
I��
1 Z0 -�
= r-�
16-5 ���
�—�~
16A
5 10 15 20 25 30 35 40 45 50 55 60 65
Total Discharge(cfs)
Water Surface Profile Plot for Culvert: Culvert 1
Crossui�-Black-wood RD.Desi�i Dischar�e - 16.0 cfs
� Cuh�ert-Cuh�ert 1.Culcert Discharae-16_0 cfs�
22
21
20
�19
0
m �
a�i
W �$
17
_____�
16
15
-20 0 20 40 60 80 100 120 140
Station(ft)
Site Data - Culvert 1
Site Data Option: Culvert Invert Data
Inlet Station: 0.00 ft
Inlet Elevation: 17.06 ft
Outlet Station: 108.00 ft
Outlet Elevation: 15.16 ft
1Vumber of Barrels: 1
Culvert Data Summary - Culvert 1
Barrel Shape: Pipe Arch
Barrel Span: 43.75 in
Barrel Rise: 26.62 in
Barrel Material: Concrete
Embedment: 0.00 in
Barrel Manning's n: 0.0130
Culvert Type: Straight
Inlet Configuration: Square Edge with Headwall (Ke=0.5)
Inlet Depression: None
Tailwater Data for Crossing: Blackwood RD
Table 2- Downstream Channel Rating Curve(Crossing: Blackwood RD)
Flow(cfs) Water Velocity Depth (ft) Shear(pst� Froude
Surface (ft/s) Number
Elev(ft)
7.46 16.22 1.06 2.38 0.99 0.83
10.86 16.31 1.15 2.40 1.07 0.84
14.25 16.37 1.21 2.49 1.13 0.85
16.00 16.40 1.24 2.54 1.16 0.85
21.04 16.46 1.30 2.67 1.22 0.86
24.44 16.50 1.34 2.75 1.25 0.87
27.84 16.53 1.37 2.83 1.28 i 0.88 �
31.23 16.56 1.40 2.90 1.31 0.88
34.63 16.59 1.43 2.96 1.33 * 0.89 �
38.02 16.61 1.45 3.02 1.36 0.89
41.42 16.64 1.48 3.08 1.38 0.90
Tailwater Channel Data - Blackwood RD
Tailwater Channel Option: Irregular Channel
Channel Slope: Irregular Channel
User Defined Channel Cross-Section
Coord No. Station (ft) Elevation (ft) Manning's n
1 0.00 18.78 0.0300
2 62.84 16.18 0.0300
3 � 65.11 15.16 � 0.0300 �
4 66.71 15.99 0.0300
5 141.09 18.19 0.0000
Roadway Data for Crossing: Blackwood RD
Roadway Profile Shape: Constant Roadway Elevation
Crest Length: 200.00 ft
Crest Elevation: 22.00 ft
Roadway Surface: Paved
Roadway Top Width: 30.00 ft
Crossing Discharge Data
Discharge Selection Method: Specify Minimum, Design,and Maximum Flow
Minimum Flow: 7.46 cfs
Design Flow: 16.00 cfs
Maximum Flow: 41.42 cfs
Table 3-Summary of Culvert Flows at Crossing:Ainsworth DR
Headwater Total Culvert 2 Roadway Iterations
Elevation (ft) Discharge Discharge Discharge
(cfs) (cfs) (cfs)
97.37 7.46 7.46 0.00 1
97.58 10.86 10.86 0.00 1
97.79 i 14.25 i 14.25 i 0.00 i 1 �
97.91 16.00 16.00 0.00 1
98.23 * 21.04 * 21.04 * 0.00 * 1 �
98.45 24.44 24.44 0.00 1
98.69 27.84 27.84 0.00 1
98.93 31.23 31.23 0.00 1
99.18 i 34.63 i 34.63 i 0.00 i 1 �
99.44 38.02 38.02 0.00 1
99.72 41.42 * 41.42 * 0.00 * 1
102.00 63.67 63.67 0.00 Overtopping
Rating Curve Plot for Crossing:Ainsworth DR
Total Ratui�Cuive
Croccina.�inc���orth DR
102.0
101.5
101_0
�100_5
c
0
� 100.0
a�
w
°' gg 5
m
3
�
m
= 99-0
98.5
98A
97.5
5 10 15 20 25 30 35 40 45 50 55 60 65 70
Total Discharge(cfs)
Culvert Data: Culvert 2
Table 2-Culvert Summary Table: Culvert 2
Total Culve Head Inle Outl Fl Nor Criti Out Tailw Outl Tailw
Disch rt water t et ow mal cal let ater et ater
arge Disch Elevat Cont Cont Ty Dep Dep De Dept Velo Veloc
(cfs) arge ion rol rol pe th th pth h (ft) city ity
(cfs) (ft) Dep Dep (ft) (ft) (ft) (ft/s (ft/s)
th th )
(ft) (tt)
7.46 7.46 97.37 0.88 0.0* 1- 0.46 0.63 0.4 0.61 6.03 2.71
cfs cfs S2 6
n
10.86 10.86 97.58 1.09 0.0* 1- 0.56 0.77 0.5 0.70 6.86 2.98
cfs cfs S2 6
n
14.25 14.25 97.79 1.30 0.0* 1- 0.64 0.90 0.6 0.78 7.52 3.18
cfs cfs S2 4
n
16.00 16.00 97.91 1.42 0.0* 1- 0.69 0.96 0.6 0.81 7.81 3.28
cfs cfs S2 9
n
21.04 21.04 98.23 1.74 0.26 1- 0.80 1.12 0.8 0.91 8.37 3.43
cfs cfs 5 S2 1
n
24.44 24.44 98.45 1.96 0.51 1- 0.88 1.22 0.8 0.98 8.75 3.36
cfs cfs 0 S2 9
n
27.84 27.84 98.69 2.20 0.77 1- 0.95 1.32 0.9 1.05 9.05 3.28
cfs cfs 0 S2 7
n
31.23 31.23 98.93 2.44 1.04 5- 1.02 1.41 1.0 1.10 9.36 3.21
cfs cfs 7 S2 4
n
34.63 34.63 99.18 2.69 1.34 5- 1.09 1.49 1.1 1.14 9.62 3.19
cfs cfs 0 S2 2
n
38.02 38.02 99.44 2.95 1.65 5- 1.17 1.57 1.2 1.18 9.86 3.20
cfs cfs 0 S2 0
n
41.42 41.42 99.72 3.23 1.97 5- 1.24 1.65 1.2 1.21 10.0 3.22
cfs cfs 6 S2 7 7
n
*Full Flow Headwater elevation is below inlet invert.
Culvert Barrel Data
Culvert Barrel Type Straight Culvert
Inlet Elevation (invert): 96.49 ft,
Outlet Elevation (invert): 95.22 ft
Culvert Length: 104.01 ft,
Culvert Slope: 0.0122
Culvert Performance Curve Plot: Culvert 2
PerfoiYuance Curve
c,��� c,�n��c�
0 0
Inlet Control Elev Outlet Control Elev
102.0
101.5
101.0 .',
100.5 �'
i
=100_0 ��
c
� 99.5
�
a�
w 99.0
a� �
i
3 98 5 -�
� �
= 98A r
!�•
9Z5 ��
�
�
97A �
_,_--
96-5 r�
��
96.0 ��
�
5 10 15 20 25 30 35 40 45 50 55 60 65 70
Total Discharge(cfs)
Water Surface Profile Plot for Culvert: Culvert 2
Crossui�-Auisworth DR.Desi�i Dischar�e - 16.0 cfs
� Cuh�ert-Ciilc�ert?.Cuh�ert Discharae-16_0 cfs�
102
101
100
� 99
0
m
a�i
w gg +
97 --- - -_ - - - - -___
96 =____�
95
-20 0 20 40 60 80 100 120
Station(ft)
Site Data - Culvert 2
Site Data Option: Culvert Invert Data
Inlet Station: 0.00 ft
Inlet Elevation: 96.49 ft
Outlet Station: 104.00 ft
Outlet Elevation: 95.22 ft
1Vumber of Barrels: 1
Culvert Data Summary - Culvert 2
Barrel Shape: Pipe Arch
Barrel Span: 43.75 in
Barrel Rise: 26.62 in
Barrel Material: Concrete
Embedment: 0.00 in
Barrel Manning's n: 0.0130
Culvert Type: Straight
Inlet Configuration: Square Edge with Headwall (Ke=0.5)
Inlet Depression: None
Tailwater Data for Crossing: Ainsworth DR
Table 4- Downstream Channel Rating Curve(Crossing:Ainsworth DR)
Flow(cfs) Water Velocity Depth (ft) Shear(pst� Froude
Surface (ft/s) Number
Elev(ft)
7.46 95.83 0.61 2.71 0.57 0.86
10.86 95.92 0.70 2.98 0.66 0.88
14.25 96.00 0.78 3.18 0.73 0.90
16.00 96.03 0.81 3.28 0.76 0.91
21.04 96.13 0.91 3.43 0.85 0.92
24.44 96.20 0.98 3.36 0.92 0.91
27.84 96.27 1.05 3.28 0.98 i 0.91 �
31.23 96.32 1.10 3.21 1.03 0.91
34.63 96.36 1.14 3.19 1.07 * 0.91 �
38.02 96.40 1.18 3.20 1.10 0.91
41.42 96.43 1.21 3.22 1.13 0.91
Tailwater Channel Data - Ainsworth DR
Tailwater Channel Option: Irregular Channel
Channel Slope: Irregular Channel
User Defined Channel Cross-Section
Coord No. Station (ft) Elevation (ft) Manning's n
1 44.14 97.55 0.0300
2 99.23 96.24 0.0300
3 � 112.85 i 95.22 � 0.0300 �
4 114.08 96.11 0.0300
5 180.74 98.24 0.0000
Roadway Data for Crossing: Ainsworth DR
Roadway Profile Shape: Constant Roadway Elevation
Crest Length: 200.00 ft
Crest Elevation: 102.00 ft
Roadway Surface: Paved
Roadway Top Width: 30.00 ft
Crossing Discharge Data
Discharge Selection Method: Specify Minimum, Design,and Maximum Flow
Minimum Flow: 7.46 cfs
Design Flow: 16.00 cfs
Maximum Flow: 41.42 cfs
Table 5-Summary of Culvert Flows at Crossing: Parkway AVE
Headwater Total Culvert 3 Roadway Iterations
Elevation (ft) Discharge Discharge Discharge
(cfs) (cfs) (cfs)
82.98 7.46 7.46 0.00 1
83.19 10.86 10.86 0.00 1
83.41 i 14.25 i 14.25 i 0.00 i 1 �
83.52 16.00 16.00 0.00 1
83.84 * 21.04 * 21.04 * 0.00 * 1 �
84.07 24.44 24.44 0.00 1
84.30 27.84 27.84 0.00 1
84.54 31.23 31.23 0.00 1
84.79 i 34.63 i 34.63 i 0.00 i 1 �
85.05 38.02 38.02 0.00 1
85.33 * 41.42 * 41.42 * 0.00 * 1
88.00 66.72 66.72 0.00 Overtopping
Rating Curve Plot for Crossing: Parkway AVE
Total Ratui�Cuive
Crocc�a Park-���ac.�\'E
88.0
8Z5
87.0
86_5
C
� 86-0
m
�
a�
w 85.5
a�
m
� 85-0
m
a�
S
84_5
84.0
83.5
83_0
10 20 30 40 50 60 70
Total Dfscharge(cfs)
Culvert Data: Culvert 3
Table 3-Culvert Summary Table: Culvert 3
Total Culve Head Inle Outl Fl Nor Criti Out Tailw Outl Tailw
Disch rt water t et ow mal cal let ater et ater
arge Disch Elevat Cont Cont Ty Dep Dep De Dept Velo Veloc
(cfs) arge ion rol rol pe th th pth h (ft) city ity
(cfs) (ft) Dep Dep (ft) (ft) (ft) (ft/s (ft/s)
th th )
(ft) (tt)
7.46 7.46 82.98 0.87 0.0* 1- 0.42 0.63 0.4 0.67 6.83 2.69
cfs cfs S2 2
n
10.86 10.86 83.19 1.08 0.0* 1- 0.51 0.77 0.5 0.76 7.76 2.90
cfs cfs S2 1
n
14.25 14.25 83.41 1.30 0.0* 1- 0.58 0.90 0.5 0.83 8.51 3.08
cfs cfs S2 8
n
16.00 16.00 83.52 1.41 0.0* 1- 0.62 0.96 0.6 0.87 8.85 3.16
cfs cfs S2 2
n
21.04 21.04 83.84 1.73 0.0* 1- 0.72 1.12 0.7 0.95 9.47 3.36
cfs cfs S2 3
n
24.44 24.44 84.07 1.96 0.0* 1- 0.78 1.22 0.8 1.00 9.76 3.48
cfs cfs S2 1
n
27.84 27.84 84.30 2.19 0.01 1- 0.85 1.32 0.8 1.05 10.5 3.59
cfs cfs 1 S2 5 9
n
31.23 31.23 84.54 2.43 0.29 5- 0.91 1.41 0.9 1.09 10.5 3.69
cfs cfs 5 S2 4 2
n
34.63 34.63 84.79 2.68 0.59 5- 0.97 1.49 1.0 1.13 10.9 3.78
cfs cfs 7 S2 0 4
n
38.02 38.02 85.05 2.94 0.91 5- 1.03 1.57 1.0 1.16 11.1 3.86
cfs cfs 7 S2 7 3
n
41.42 41.42 85.33 3.22 1.25 5- 1.09 1.65 1.1 1.20 11.3 3.94
cfs cfs 4 S2 3 7
n
*Full Flow Headwater elevation is below inlet invert.
Culvert Barrel Data
Culvert Barrel Type Straight Culvert
Inlet Elevation (invert): 82.11 ft,
Outlet Elevation (invert): 80.05 ft
Culvert Length: 116.02 ft,
Culvert Slope: 0.0178
Culvert Performance Curve Plot: Culvert 3
PerfoiYuance Cuive
Cuh�ert Culc�ert 3
0 0
Inlet Control Elev Outlet Control Elev
88
87
i,
�86
c �
o �
� 85 _-
� -
a�
w
� 84
� .-
� .
m �
a� �
= 83 �1�
��
��
82 _���
��
�
s� �_r—r
10 20 30 40 50 60 70
Total Discharge(cfs)
Water Surface Profile Plot for Culvert: Culvert 3
Crossui�- Park-way A`�E.Desi�i Dischar�e - 16.0 cfs
Cuh�ert-Cuh�ert 3.Cuh�ert Discharae-16_0 cfs
88
87
86
85
c
� 84
�
a� +
w
83
82 ---- ----
81 =____�
80
-20 0 20 40 60 80 100 120 140
Station(ft)
Site Data - Culvert 3
Site Data Option: Culvert Invert Data
Inlet Station: 0.00 ft
Inlet Elevation: 82.11 ft
Outlet Station: 116.00 ft
Outlet Elevation: 80.05 ft
1Vumber of Barrels: 1
Culvert Data Summary - Culvert 3
Barrel Shape: Pipe Arch
Barrel Span: 43.75 in
Barrel Rise: 26.62 in
Barrel Material: Concrete
Embedment: 0.00 in
Barrel Manning's n: 0.0130
Culvert Type: Straight
Inlet Configuration: Square Edge with Headwall (Ke=0.5)
Inlet Depression: None
Tailwater Data for Crossing: Parkway AVE
Table 6- Downstream Channel Rating Curve(Crossing: Parkway AVE)
Flow(cfs) Water Velocity Depth (ft) Shear(pst� Froude
Surface (ft/s) Number
Elev(ft)
7.46 80.72 0.67 2.69 0.62 0.87
10.86 80.81 0.76 2.90 0.71 0.88
14.25 80.88 0.83 3.08 0.78 0.90
16.00 80.92 0.87 3.16 0.81 0.90
21.04 81.00 0.95 3.36 0.89 0.92
24.44 81.05 1.00 3.48 0.94 0.93
27.84 81.10 1.05 3.59 0.98 i 0.93 �
31.23 81.14 1.09 3.69 1.02 0.94
34.63 81.18 1.13 3.78 1.05 * 0.95 �
38.02 81.21 1.16 3.86 1.09 0.95
41.42 81.25 1.20 3.94 1.12 0.96
Tailwater Channel Data - Parkway AVE
Tailwater Channel Option: Irregular Channel
Channel Slope: Irregular Channel
User Defined Channel Cross-Section
Coord No. Station (ft) Elevation (ft) Manning's n
1 0.00 83.55 0.0300
2 30.00 80.55 0.0300
3 � 33.00 80.05 � 0.0300 �
4 36.00 80.55 0.0300
5 66.00 83.55 0.0000
Roadway Data for Crossing: Parkway AVE
Roadway Profile Shape: Constant Roadway Elevation
Crest Length: 200.00 ft
Crest Elevation: 88.00 ft
Roadway Surface: Paved
Roadway Top Width: 30.00 ft
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