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Surface Runoff Model for Navajo Reservoir Solaleh Khezri Spring 2010

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Surface Runoff Model for Navajo Reservoir Solaleh Khezri Spring 2010. Navajo Reservoir. Drainage Area : 3190 Sq mi Located on San Juan River Dam Construction was completed in 1962. HEC-HMS Model. Basin Component Represent the physical Watershed Meteorological Component - PowerPoint PPT Presentation
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Surface Runoff Model for Navajo Reservoir Solaleh Khezri Spring 2010
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Page 1: Surface Runoff Model  for Navajo Reservoir  Solaleh  Khezri Spring 2010

Surface Runoff Model for Navajo Reservoir Solaleh KhezriSpring 2010

Page 2: Surface Runoff Model  for Navajo Reservoir  Solaleh  Khezri Spring 2010

Navajo Reservoir

• Drainage Area : 3190 Sq mi• Located on San Juan River• Dam Construction was completed in 1962.

Page 3: Surface Runoff Model  for Navajo Reservoir  Solaleh  Khezri Spring 2010

HEC-HMS ModelBasin ComponentRepresent the physical WatershedMeteorological ComponentSpecifies the precipitation input for a sub-basin elementControl SpecificationDefine the duration and time step of the simulation

run

Page 4: Surface Runoff Model  for Navajo Reservoir  Solaleh  Khezri Spring 2010

Basin Model Digital Elevation Map

Watershed

Delineation (Arc Hydro)

Basin Processing (Geo-HMS)

Import

the Basi

n Model to HEC

-HMS

Longest Flow Path

Basin Centroid

Basin Slope

Basin Lag time

Centroidal Flow PathAdd HMS Schematic/Legend

Page 5: Surface Runoff Model  for Navajo Reservoir  Solaleh  Khezri Spring 2010

Some Tricks about Geo-HMSClean the local Temp directory, before using

HEC-GeoHMS tool in ArcGIS.

The Subbasin Centroid may falls on the subbasin boundary.

Page 6: Surface Runoff Model  for Navajo Reservoir  Solaleh  Khezri Spring 2010

Basin Model

Page 7: Surface Runoff Model  for Navajo Reservoir  Solaleh  Khezri Spring 2010

Basin Model Elements Junction: Combines streamflow from

elements located upstream of a junction.

Reach: Convey streamflow in the basin model.

Subbasin: Represent the physical Watershed.

Reservoir: Models the detention or attenuation of a hydrograph.

Page 8: Surface Runoff Model  for Navajo Reservoir  Solaleh  Khezri Spring 2010

Calculation Methods and Parameters

Reach • Routing Method• X=.2• K=L/V (V=1 ft/s) Loss - Gain Method

Subbasin• Loss Method (CN=60)• Transform Method (lag time calculated by HEC-Geo HMS) • Baseflow Method

Page 9: Surface Runoff Model  for Navajo Reservoir  Solaleh  Khezri Spring 2010

Meteorological Component

SCS Design Storm: rainfall intensities are arranged to maximize the peak runoff for a given total storm depth.

100 year 24 hours rainfall (4 in)

Page 10: Surface Runoff Model  for Navajo Reservoir  Solaleh  Khezri Spring 2010

Running HEC-HMS

Page 11: Surface Runoff Model  for Navajo Reservoir  Solaleh  Khezri Spring 2010

Global Summery Results

Page 12: Surface Runoff Model  for Navajo Reservoir  Solaleh  Khezri Spring 2010

Result for an Element

Page 13: Surface Runoff Model  for Navajo Reservoir  Solaleh  Khezri Spring 2010

Subbasin OutflowLag

Time: 442 min

Lag Time:

740 min

Page 14: Surface Runoff Model  for Navajo Reservoir  Solaleh  Khezri Spring 2010

Future WorkRun the model for a specific precipitation

event Compare the outflow with the observed

streamflowWrite a Report


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