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Hydrogroup Meeting Mohid Land & Mohid Drainage Network. Frank Braunschweig Rosa Trancoso Pedro Galvão Pedro Chambel Ramiro Neves Etc. Presentation Overview. Introduction Mohid Framework Mohid Land vs. Mohid Drainage Network Pardiela (Degebe) Catchment Characteristics
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Hydrogroup MeetingMohid Land & Mohid Drainage Network Frank Braunschweig Rosa Trancoso Pedro Galvão Pedro Chambel Ramiro Neves Etc.
Presentation Overview • Introduction • Mohid Framework • Mohid Land vs. Mohid Drainage Network • Pardiela (Degebe) Catchment Characteristics • Mohid Drainage Network • Channel Flow Results • Heat Fluxes • Coliform Decay • Channel Bed Water Exchange • Pool Implementation • Cascade Incorporation • SWAT Coupling • Cohesive Sediment Transport • Coupling Water Quality Modules • Mohid Land • Spatial Rainfall Interpolation • Future Tasks
Introduction MOHID Water Modeling System - Numerics MOHID Soil MOHID Land Executable Macrospore, Soil, … Runoff, Basin, … Library MOHID Water Mohid Base 3 Soil modules Basin Delineator Digital Terrain Creator Module Hydrodynamic, Waterproperties, … Soil, Soil Properties,... Convert To XYZ Convert To HDF 5 Mohid Base 2 Grid and Atmosphere modules River Network Horizontal Grid, Vertical Grid, Atmosphere, Advection Diffusion, ... Mohid Base 1 Process, IO and Function modules Global Data, Water Quality, Sediment Quality, EnterData, HDF, Functions, Time, LUD, Triangulation, Time Series, ...
1D Drainage network 2D Overland flow Precipitation Variable in Time & Space 3D Porous Media Introduction Mohid Land vs. Mohid Drainage Network Mohid Drainage Network – Standalone program which simulates in-stream processes. Data not provided simulated by the model must be supplied as boundary condition (e.g. overland flow discharge) Mohid Land – Integrated Model composed by a set of modules (Overland flow, Drainage Network, Atmosphere, Porous Media, etc.)
Introduction Catchment Caracteristics Source: NASA & Mohid GIS Source: Textural Map & Saxon 1986 Source: Land Use & Ponce, 1989, p. 139
Introduction Catchment Caracteristics Minimum water depth for flow: 0.001m
Introduction Catchment Caracteristics Initial Water content = Field capacity 8 Vertical Layers
MOHID Drainage Network Channel Flow Results • Delivery Model MOHID Land: • Run 06 – Manning Channels = 0.03, Rain Constant in Space • Run 08 – Manning Channels = 0.03, Rain Variable in Space • Run 10 – Manning Channels = 0.06, Rain Variable in Space
MOHID Drainage Network Channel Flow Results Run 06 – Manning Channels = 0.03, Rain Constant in Space Run 08 – Manning Channels = 0.03, Rain Variable in Space Run 10 – Manning Channels = 0.06, Rain Variable in Space Second Event recorded by probe First Event recorded by probe
Results – Total Mass EVTP Infiltration Rain Flow
MOHID Fill MatrixRain Interpolation Delaunay triangulation Inverse Weight Distance Produces HDF Files with a Matrix of Rainfall (or any other property) with a user defined frequency (e.g. 1 hour) during a user defined period (e.g. 2003-2004)
MOHID LandRain Interpolation Rain Stations Overland Flow Channel Flow Relative Water Content in the upper soil layer
Solar Radiation (Date, Hour of Day, Cloud Cover, Riparian Shading) Sensible Heat (Wind, Water & Air Temperature) Long wave Radiation (Cloud Cover, Water & Air Temperature) Latent Heat (Water & Air Temperature, Wind Speed, Relative Humidity) Sediment Exchange (Water & Sediment Temperature) MOHID Drainage Network Heat Fluxes • Input Variables: • Air Temperature • Wind Speed • Relative Humidity • Cloud Cover • Riparian Shading Equations From Water Temperature Modeling Review Central Valley September 2000 Michael L. Deas Cindy L. Lowney
MOHID Drainage Network Heat Fluxes • Input Variables: • Air Temperature –Hourly Data • Wind Speed – Hourly Data • Relative Humidity – Daily Data • Cloud Cover – Monthly Invented Data • Riparian Shading – Constant Coefficient of 70%
Solar Radiation (Date, Cloud Cover, Riparian Shading) MOHID Drainage Network Coliform Bacteria Coliform Decay (Water Temperature, Salinity & Radiation) • Input Variables: • T90 Method • T90 Computation Methods • Constant • Canteras • Chapra
MOHID Drainage Network Coliform Bacteria Discharges = 0.25m3/s Initial Concentration = 1.e7 u/100ml
MOHID Land Channel Bed Water Exchange Channel – Water Table Exchange Overland Flow - Channel Channel - Overland Flow (Floods) Calculation based on the hydraulic head gradient
MOHID Drainage Network Pool Implementation Top Width Channel Height Water Depth Pool Depth Bottom Width Node Volume = + Area Vertical =
MOHID Drainage Network Pool Implementation Discharges = 0.10m3/s Conclusion: With Pools water level rises later but quicker at the outlet Pools (Initially empty)
<30min. MOHID Drainage Network Pool Implementation Sediment Concentration
Deposition Erosion MOHID Drainage Network Cohesive Sediment Transport - Equations tero* – Critical Erosion shear stress E – Erosion constant [5e-4 kg m-2 s-1] tdep* – Critical Deposition shear stress C – Suspended concentration [kg m-3] Ws – Settling velocity [m s-1] HS – Hindered settling
MOHID Drainage Network Cohesive Sediment Transport - Test • Daily precipitation • No suspended sediment
1. WASP MOHID Drainage Network Coupling Water Quality Modules Water Quality (WASP) Ce-Qual-W2 Coupled Module Water Quality Each River Reach is a control Volume In each Time Step Concentration are passed to the Water Quality Model Based on Concentration and Rates these modules calculate new Concentrations Water Quality Modules pass back new concentrations to River Reaches
1. WASP MOHID Land Coupling Water Quality Modules • Results so far don’t make sense • Wrong boundary conditions (Constant concentration from Overland / Groundwater) • Maybe wrong parameterization
time ? t+1 t downstream MOHID Drainage Network Cascade Integration - Equations • Continuity • Momentum Kinematic Wave:
MOHID Drainage Network Cascade Integration - Algorithm Conservativemethod! Volume Depth, Area Flow Yes New Volume Error = Vol – New Vol Error > Tolerance?
MOHID Drainage Network Cascade Integration - Results Equal! Min DT = 10s MOHID Test for stability: Not Equal: Higher DT gives higher peak Min DT = 12.5s Equal! Min DT = 13.63s Conclusion: Cascade gives more correct results for higher DTs
MOHID Drainage Network SWAT Coupling – Task 1 • SWAT code changed to produce a discharge file for each subbasin outlet Outlet of Sub-Basin 1 Outlet of Sub-Basin 11
MOHID Drainage Network SWAT Coupling – Task 2 • Import to MOHID GIS ArcView File with the location of the outlets of the sub-basin
MOHID Drainage Network SWAT Coupling – Task 3 • Produce a Discharge Input file for Mohid Drainage Network
MOHID Drainage NetworkSWAT Coupling – Task 4 • Run MOHID Drainage Network with discharges from SWAT
Comparison SWAT (Integrated Model) vs. MOHID Drainage Network (using SWAT as delivery model) MOHID Drainage Network SWAT Coupling – Task 4
Comparison Mohid Land (Integrated Model) vs. MOHID Drainage Network (using SWAT as delivery model) MOHID Drainage Network SWAT Coupling – Task 4
MOHID Porous Media Features • 3D non saturated flow • 2D aquifer • Two new vertical coordinates • Sigma Top • Cartesian Top • Dynamic Interface between 2D and 3D zone • Will be presented by Pedro Galvão…
Mohid LandFuture Tasks To Do In Progress Done