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Learn about hydrologic models and geographic information system tools for watershed analysis, including the impact of land use changes on retention and the use of GIS for organizing and synthesizing multiple data sources.
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Hydrologic Modeling for Watershed Analysis and River Restoration David Tarboton http://www.engineering.usu.edu/dtarb/ dtarb@cc.usu.edu
Learning Objectives • Review what you learned yesterday • be familiar with the sources for hydrologic, hydrographic and watershed data useful for watershed analysis • be familiar with hydrologic models and geographic information system tools useful for watershed analysis • be familiar with geomorphologic models for landslides, erosion and calculation of sediment inputs • questions to ask when applying or looking at results from a watershed model
P ET Gin Q S Gout The role of watershed processes in runoff and sediment production Short time scale water balance Retention How do watershed land use changes impact retention?
SCS Curve Numbers to Quantify Retention CN=100 80 90 70 60 50 40 30 20
Grid based terrain flow data model Grid network Eight direction pour point model D8 4 3 2 1 1 1 1 1 5 6 7 1 1 4 3 3 1 8 1 2 1 1 12 Drainage Area 1 1 1 2 16 2 1 3 6 25
Key Take Home Message • The GIS grid based terrain flow data model enables the representation of flow processes at and near the earth surface and derivation of a wide variety of information useful for the study of hydrologic processes.
What you learned in the exercise • ArcGIS, Bare Essentials • To learn more see http://www.esri.com, http://campus.esri.com/, http://www.engineering.usu.edu/dtarb/giswr/. • Watershed delineation using TauDEM • To learn more see http://www.engineering.usu.edu/dtarb/taudem. • http://www.engineering.usu.edu/dtarb/giswr/2005/LoganRiverExercise.htm
GIS provides an effective way to organize and synthesize multiple data sources and compute watershed attributes
Some Cub River GIS Watershed Analysis Findings • Watershed Area 146.9 x 106 m2 = 57.4 mi2 (c.f. USGS gauge area 53.7 mi2) • PRISM Mean Annual Precipitation 650 mm = 25.6 in.
More Cub River Watershed Analysis Findings • USGS Mean Annual Streamflow based on 12 years of data, 1940-1952: 64.6 cfs
More Cub River Watershed Analysis Findings StreamStats Regional Regression Hortness, J. E., and Berenbrock, C, 2001, Estimating Monthly and Annual Streamflow Statistics at Ungaged Sites in Idaho: U.S. Geological Survey Water Resources-Investigations Report 01-4093, 36 p. Uncertainty !!
We did not get to • Flow distance to streams
We did not get to • Raster Calculation [cubiddist] < 200
We did not get to • Land Cover tabulation in buffer zone
Roles for Hydrologic Models • Make predictions (of the future) • Quantify and test theories • Evaluate potential outcomes from management alternatives
Watershed restoration limitations • Human population growth • Land use • Topography • Climate
Realistic Watershed management / alteration / restoration options • Best management practices • Buffer strips • Zoning • Flow (de) regulation
Data Sources for Quantification of model inputs and management alternatives • Climate • Geospatial
Hydrology Data Layers Streams Drainage Areas Hydrography Channels Terrain Surfaces Rainfall Digital orthophotos
National Hydro Data Programs National Elevation Dataset (NED) National Hydrography Dataset (NHD) http://seamless.usgs.gov/ http://nhd.usgs.gov/ NED-Hydrology Watershed Boundary Dataset http://edcnts12.cr.usgs.gov/ned-h/index.html
http://seamless.usgs.gov/ DEMs NLCD NHD Topographic Maps
National Land Cover Dataset http://landcover.usgs.gov/nationallandcover.html Get the data: http://seamless.usgs.gov/
USGS National Water Information System Web access to USGS water resources data in real time http://waterdata.usgs.gov/usa/nwis/
1:250,000 Scale Soil Information http://www.ftw.nrcs.usda.gov/stat_data.html
SSURGO (Soil Survey Geographic Database) developed, maintained and available online (soildatamart.nrcs.usda.gov ) by the U.S. Department of Agriculture (USDA) Natural Resources Conservation Service (NRCS)
Regional Watershed Information Systems http://www.bearriverinfo.org/
Specialized data collection e.g. LIDAR 3-D detail of the Tongue river at the WY/Mont border from LIDAR. Roberto Gutierrez University of Texas at Austin
Models for Hydrology and Runoff • Rational Formula Q = C I A • Unit Hydrographs - HECHMS • Continuous Water and Sediment Simulation - EPA BASINS (HSPF and SWAT) • TOPMODEL • DHSVM
HEC-HMS Assumptions and Methods • A basin model is constructed by connecting elements comprising • Precipitation Input • Subbasin • Runoff Volume (Infiltration model, e.g. SCS CN, Green-Ampt) • Direct Runoff (Unit Hydrograph) • Baseflow • Reach • Junction • Source • Sink • Reservoir • Diversion
HSPF Comprehensive time series based simulation system designed to accommodate a wide variety of simulation modules
Soil and Water Assessment Tool (SWAT) • Continuous time Daily Water Balance Simulation • Developed to predict the impact of land management practices on water, sediment and agricultural chemical yields • Physically based • Includes • Climate - weather generator • Snow • Soil temperature • Canopy storage • Infiltration • Evaporation • Erosion (MUSLE)
TOPMODEL Beven, K., R. Lamb, P. Quinn, R. Romanowicz and J. Freer, (1995), "TOPMODEL," Chapter 18 in Computer Models of Watershed Hydrology, Edited by V. P. Singh, Water Resources Publications, Highlands Ranch, Colorado, p.627-668. “TOPMODEL is not a hydrological modeling package. It is rather a set of conceptual tools that can be used to reproduce the hydrological behaviour of catchments in a distributed or semi-distributed way, in particular the dynamics of surface or subsurface contributing areas.”
TOPMODEL Key Ideas • Surface saturation and soil moisture deficits based on topography • Slope • Specific Catchment Area • Topographic Convergence • Partial contributing area concept • Saturation from below (Dunne) runoff generation mechanism
DHSVM http://www.hydro.washington.edu/Lettenmaier/Models/DHSVM/ • Distributed Hydrology-Soil-Vegetation Model • Physically based hydrologic model • Grid-based (DEM) • Two layer canopy for vegetation • Hydrologic effects of vegetation change and forest roads
Sediment Production • USLE, MUSLE, RUSLE2, … (http://www.ars.usda.gov/Research/docs.htm?docid=6010) • SINMAP (http://www.engineering.usu.edu/dtarb/sinmap.htm) • SHALSTAB (http://ist-socrates.berkeley.edu/~geomorph/shalstab/)
USLE The Universal Soil Loss Equation A = RKLSCP, where, A = soil loss per unit area (t/ha) R = Rainfall-Runoff erositivity (Mj*mm/ha*h*yr) K = Soil erodibility (t*ha*h/ha*Mj*mm) L = Slope length factor S = Slope steepness factor C = Crop (land cover) factor P = Practice (erosion controls) factor
SINMAP - Terrain Stability Mapping With Bob Pack. http://www.engineering.usu.edu/dtarb/sinmap.htm
Questions to ask about models(What it does) • Are the physics representative of processes in my watershed? • How were the parameters obtained? • Calibration • Out of sample validation (split sample or cross validation) • Reference (lookup based on other attributes) • What are the inputs? • What are the outputs?
Questions to ask about models contd.. (Error) • What are the sources of error • Model structural error (differences between physical reality and model equations) • Input data errors • Parameter errors • What is the uncertainty in the inputs? • How does input uncertainty propagate through to the results? • What is the uncertainty in the outputs?