1 Overview of Unsteady Flow Modeling With HEC-RAS Gary W. Brunner, P.E.

Slides:



Advertisements
Similar presentations
Flood Profile Modeling with Split Flows and Weirs
Advertisements

L-1621/Klipsch98 1 Importing HEC-2 Data Into HEC- RAS What you need to know…
Dynamic Floodways: Accounting for Both Storage and Conveyance José María Guzmán, P.E. Gaston Cabanilla, P.E., CFM May 2010, National ASFPM Conference,
Use of a hydrodynamic model to
HYDROLOGIC AND HYDRAULIC MODELING Hydrologic Precipitation & Basin Parameters, Flood Frequency Analysis Hydraulic Energy & Momentum Relationships.
CHAPTER FOUR Stream flow measurement
Streamflow and Runoff The character, amount, and timing of discharge from a basin tells a lot about flow paths within the basin Therefore, important to.
US Army Corps of Engineers BUILDING STRONG ® Methods for Determining Maximum Flood Elevations Landward of Failed Levees: An Example from the Great Missouri.
1 Sediment Management for Dam Removal: An HEC-6 Approach.
Alluvial Fan Flood Hazard Mapping and Dam Failure Analysis using USGS Diffusion Hydrodynamic Model by Neil M. Jordan, P.E. September 11, 2003.
Floodplain Mapping using HEC-RAS and ArcView GIS Eric Tate Francisco Olivera David Maidment
Processing Geospatial Data with HEC-GeoRAS 3.1
HEC-RAS US Army Corps of Engineers Hydrologic Engineering Center
Application of GIS Tools for Hydraulic Modeling
Stage – Discharge Rating Numerical relationship between water elevation (stage) and discharge at a location in a flowing system. Expressed as an equation,
CEE 795 Water Resources Modeling and GIS Learning Objectives: Describe the HEC-River Analysis System (RAS) Model Utilize HEC Geo-RAS to import data into.
HEC-RAS.
Modeling River Ice and River Ice Jams with HEC-RAS
Evaluating river cross section for SPRINT: Guadalupe and San Antonio River Basins Alfredo Hijar Flood Forecasting.
Texas A&M University, Department of Civil Engineering CVEN 689 Applications of GIS in Civil Engineering Professor: Dr. Francisco Olivera Student: Brad.
CEE 795 Water Resources Modeling and GIS Learning Objectives: Utilize advanced features in HEC Geo-RAS Handouts: Assignments: Exercise #7 Lecture 8: Advanced.
WinTR-20 Project Formulation Hydrology Computer Program Basic Input and Output Presented by: WinTR-20 Development Team.
WinTR-20 Project Formulation Hydrology Computer Program Basic Input and Output Presented by: WinTR-20 Development Team.
CH 7 - Open Channel Flow Brays Bayou Concrete Channel Uniform & Steady
Solution of the St Venant Equations / Shallow-Water equations of open channel flow Dr Andrew Sleigh School of Civil Engineering University of Leeds, UK.
1D Steady State Hydraulic Modelling Bratton Stream Case Study.
Feb 2003HEC-RAS Version 3.11 Slides adapted from HEC Unsteady Flow Course Unsteady Flow Course.
Hydraulic Engineering
MVS Mainstem Forecast Model Update: NETMISS2 by Joel Asunskis, P.E. Hydraulic Engineer, St. Louis District Water Control U.S. Army Corps Of Engineers October.
by David M. Beekman and Vito A. Cimino
Building a model step by step. MIKE 11 requires information on : Catchment data (Surface- root- and groundwater zones). River Network i.e. Branches; Nodes;
WinTR-20 Advanced Features March WinTR-20 Project Formulation Hydrology Computer Program Advanced Features Presented by: WinTR-20 Development Team.
March 2009WinTR-20 Course1 Muskingum-Cunge Flood Routing Procedure in NRCS Hydrologic Models Prepared by William Merkel USDA-NRCS National Water Quality.
__________________________ SITES INTEGRATED DEVELOPMENT ENVIRONMENT for WATER RESOURCE SITE ANALYSIS COMPLEX WATERSHEDS SITES IN SERIES.
WinTR-20 Project Formulation Hydrology Computer Program Overview Presented by: WinTR-20 Development Team.
Channel Design Channel design based on use of Manning eq. to find normal depth Yo for a specified discharge. Using Manning eq. M = 1.49 imperial 1.00 metric.
HEC-RAS Version 3.1 Basic Input Lecture 3 Presented by:
Channel Flow Routing Reading: Applied Hydrology Sections 8.4, , 9.7.
March 2003HEC-RAS Version 3.1 Other Features of HEC-RAS- part 2 Cross Section Interpolation Multiple Plans Supporting Pictures.
Uniform Open Channel Flow
Dynamic Channel Routing Preissmann Scheme. Dynamic Channel Routing Preissmann Scheme unconditionally stable for  >=0.5 second-order accurate if 
Mathematical Background
HEC-GEORAS on a small stream in North Branch, Clear Creek Zhihao Wang Sep 2011.
Modeling Inline Structures using HEC-RAS Version 3.1
1 Triangulated Irregular Network Node Edge Face. 2 3D Structure of a TIN.
Penny Coombes Sarah Wharton Gary Davies Simon White River Bee, Desing FLOOD ALLEVIATION FEASIBILITY.
Basic Hydraulics: Channels Analysis and design – I
HEC-RAS Version 3.1 Overview
Basic Hydraulics: Open Channel Flow – I
Floodplain Management D Nagesh Kumar, IISc Water Resources Planning and Management: M8L5 Water Resources Systems Modeling.
1 INTRODUCTION TO “Stratigrafia” The code in the workbook “stratigrafia” computes - longitudinal profiles; - water surface elevation; - sediment transport.
Basic Hydrology & Hydraulics: DES 601 Module 16 Open Channel Flow - II.
Floodplain Mapping using TINs Triangulated Irregular Networks (TINs) Representation of stream channels using TINs Floodplain delineation using HEC-HMS,
April 2002HEC-RAS Version 3.0 FY02Slide 1 of 12 HEC-RAS Version 3.1 Troubleshooting.
Basic Hydraulics: Rating curve. Definition & terminology Rating curve, also known as stage–discharge curve, is a graph showing the relation between the.
Watershed Modeling using HEC-HMS and EPA-SWMM ©T. G. Cleveland, Ph.D., P.E. 25 July 2012 Lesson 14.
Basic Hydraulics: Open Channel Flow – II
Glenn E. Moglen Department of Civil & Environmental Engineering Virginia Tech End-of-semester wrap-up CEE 4324/5984 –Open Channel Flow – Lecture 27.
Basic Hydrology: Rainfall-runoff based methods – III
Basic Hydrology & Hydraulics: DES 601
Map-Based Hydrology and Hydraulics
May, 1999 Bridges This module will cover bridges and how they are input into HEC-RAS. 9/21/2018.
Distributed Flow Routing
CEE 3430 – Engineering Hydrology David Rosenberg March 26, 2012
GIS and SMS in Numerical Modeling of Open Channel Flow
UH-Downtown White Oak Buffalo.
CHAPTER FOUR Stream flow measurement
CHAPTER FOUR Stream flow measurement
CHAPTER FOUR Stream flow measurement
HEC-RAS US Army Corps of Engineers Hydrologic Engineering Center
Presentation transcript:

1 Overview of Unsteady Flow Modeling With HEC-RAS Gary W. Brunner, P.E.

2 Introduction l Overview l New Geometric Features for HEC-RAS l Geometric pre-processor l Boundary and initial conditions l Unsteady flow simulation manager l Post-processor l Additional graphics/tables to view results

3 Overview l Common geometry and hydraulic computations for steady & unsteady flow l Using the UNET equation solver (Dr. Robert Barkau) l Can handle simple dendritic streams to complex networks l Able to handle a wide variety of hydraulic structures l Extremely fast matrix solver

4 New Geometric Features for RAS l Existing Geometric Features all work for unsteady flow (XS, bridges, Culverts, inline weirs/spillways) l Lateral Weirs/Spillways l Storage Areas l Storage Area Connections (weirs, gated spillways, and culverts) l Pump Stations

5 Pre-processing Geometry l For unsteady flow, geometry is pre- processed into tables and rating curves n Cross sections are processed into tables of area, conveyance, and storage n Bridges and culverts are processed into a family of rating curves for each structure n Weirs and gated structures are calculated on the fly during unsteady flow calculations n Pre-processor results can be viewed in graphs and tables

6 Cross Section Properties Plot Property Table RS = Conveyance/1000 (cfs) Storage (cu ft) Elevation (ft) Legend Conv. Channel Conv. Valley Conv. Total Storage

7 Cross Section Properties Table

8 Bridge Hydraulic Properties Plot

9 Boundary and Initial Conditions l Boundary conditions must be established at all ends of the river system: n Flow hydrograph n Stage hydrograph n Flow and stage hydrograph n Rating curve n Normal depth

10 Boundary and Initial Conditions l Interior boundary conditions can also be defined within the river system: n Lateral inflow to a node n Uniform lateral inflow across a reach n Ground water interflow n Time series of gate openings n Elevation controlled gate n Navigation Dams n Observed internal stage and/or flow hydrograph

11 Boundary and Initial Conditions l Initial conditions must be established for the entire system: n Specify flows and perform a steady flow backwater analysis n Read in flow and stage at every node from a previous run, “hot start” file

12 Unsteady Flow Simulation Simulation Manager 1. Define a Plan 2. Select which programs to run 3. Enter a starting and ending date and time 4. Set the computation settings 5. Press the Compute button

13 HEC-RAS Computation Window Geometric Pre-Processor Unsteady Flow Simulation Post Processor Computational Messages

14 Simulation Options l Stage and Flow Output Locations l Flow Distribution Locations l Flow - Roughness Change Factors l Seasonal Roughness Factors l Friction Slope Method l Output Options: n Write out Restart File n Detailed Log level output

15 Simulation Options- Continued l Encroachments - Method 1 Only l Dam Breaching l Levee Breaching l Mixed Flow Regime l Checking Data Before Computations l Viewing Computation Log File

16 Calculation Options and Tolerances

17 Post-processing Results l Used to compute detailed hydraulic information for a set of user-specified time lines and an overall maximum water surface profile. l Computed stages and flows are passed to the steady flow program for the computation of detailed hydraulic results

18 Viewing Unsteady Flow Results l All of the output that was available for steady flow computations is available for unsteady flow (cross sections, profile, and 3D plots and tables). l Stage and flow hydrographs l Time series tables l Animation of cross section, profile and 3- dimensional graphic

19 Stage and Flow Hydrograph

20 Time Series Table

21 Animation of Profile Plot

22 HEC-RAS Demonstration