Watershed
Watershed
Watershed
1. Introduction
GIS is a powerful tool for developing solutions for water resources such as assessing water quality and managing water resources on a
local or regional scale. Hydrologists use GIS technology to integrate various data and applications into one, manageable system.
ArcGIS with Arc Hydro gives you the flexibility to combine watershed datasets from one map source with stream and river networks.
The suite of tools contained in Arc Hydro facilitate the creation, manipulation, and display of hydro features and objects within the
ArcGIS environment. Use ArcGIS Spatial Analyst for hydrologic analysis such as calculating flow across an elevation surface, which
provides the basis for creating stream networks and watersheds; calculating flow path length; and assigning stream orders.
2. OBJECTIVE
Watershed Delineation
Familiarize with the capabilities of ArcHydro.
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Step 2: Under the Customize menu of ArcMap, click the Extensions… button. You will see an extension entitled “Spatial Analyst”.
Turn on this extension.
Step 3: Go to Toolbar under the Customize menu of ArcMap, a list of tools will appear. Click the ArcHydro Tools.
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Step 5: Click on the icon to add the raster data. In the dialog box, navigate to the location of the data; select the raster file
Himachal.tif containing the DEM for Himachal Pradesh Area and click on the “Add” button.
Step 6: Click on the icon to add the vector data. In the dialog box, navigate to the location of the data; select the vector file
stream.shp containing the drainage for Himachal Pradesh Area and click on the “Add” button.
In this grid representation, water in a grid cell may flow only along one of the eight paths depicted by arrows. The number in each cell
represents the direction water travels to enter the nearest downstream cell, and the numbering scheme has been set by convention. The
numbers were determined from the series 2x x ={0,1,...7}.
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Select the appropriate Raw DEM (Himachal) and AGREE stream feature (stream).Change parameter according to following figure.
This function fills the sinks in a grid. If cells with higher elevation surround a cell, the water is trapped in that cell and cannot flow. The
Fill Sinks function modifies the elevation value to eliminate these problems.
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Confirm that the input for DEM is “AgreeDEM” (or your original DEM if Reconditioning was not implemented). The output is the
Hydro DEM layer, named by default “Fil”. This default name can be overwritten.
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Press OK. Upon successful completion of the process, the “Fil” layer is added to the map. This process takes a few minutes.
Slope Calculations with the 8-direction Pour Point Model – A) Slope calculated for diagonal cells; B) Slope calculated for cells with common sides.
Flow Direction grid, contains cells with only the numerical values dictated by the 8-direction pour point model.
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Grid Operations – A) DEM Grid; B) Flow Direction Grid. Note: Area in red is from the previous figure
Physical Representation a Flow Direction Grid –A) with directional arrows; B) As a flow network
Confirm that the input for Hydro DEM is “Fil”. The output is the Flow Direction Grid, named by default “Fdr”. This default name can
be overwritten.
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Press OK. Upon successful completion of the process, the flow direction grid “Fdr” is added to the map.
This function computes the flow accumulation grid that contains the accumulated number of cells upstream of a cell, for each cell in
the input grid. Flow accumulation grid is calculated from Flow direction grid.
Flow Accumulation – number of cells draining to a given cell (blue) along the flow network
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Confirm that the input of the Flow Direction Grid is “Fdr”. The output is the Flow Accumulation Grid having a default name of “Fac”
that can be overwritten.
Press OK. Upon successful completion of the process, the flow accumulation grid “Fac” is added to the map.
This function computes a stream grid which contains a value of "1" for all the cells in the input flow accumulation grid that have a
value greater than the given threshold. All other cells in the Stream Grid contain no data.
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Stream Definition from the Flow Accumulation Grid and a threshold value – A) Grid cells with accumulation greater than or equal to 5 are considered stream cells
(red); B) Streams identified on the flow network (red); C) Stream Grid
Confirm that the input for the Flow Accumulation Grid is “Fac”. The output is the Stream Grid. “Str” is its default name that can be
overwritten.
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A default value is displayed for the river threshold. This value represents 1% of the maximum flow accumulation: a simple rule of
thumb for stream determination threshold.
Put Number of cells “5000”. The threshold drainage area to generate a stream is then 5000 x 90 x 90 / 1000000 = 40.5 km2. A smaller
threshold will result in a denser stream network and usually in a greater number of delineated catchments.
Press OK. Upon successful completion of the process, the stream grid “Str” is added to the map.
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Stream Links defined – A) Stream Grid representation, B) Stream Links (numbers) defined, link outlets (blue), watershed outlet (red)
This function creates a grid of stream segments that have a unique identification. Either a segment may be a head segment, or it may
be defined as a segment between two segment junctions. All the cells in a particular segment have the same grid code that is specific to
that segment.
Confirm that “Fdr” and “Str” are the inputs for the Flow Direction Grid and the Stream Grid respectively. The output is the Link Grid,
with the default name “StrLnk” that can be overwritten by the user.
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Press OK. Upon successful completion of the process, the link grid “StrLnk” is added to the map.
Confirm that the input to the Flow Direction Grid and Link Grid are “Fdr” and “StrLnk” respectively. The output is the Catchment
Grid layer. “Cat” is its default name that can be overwritten by the user.
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Press OK. Upon successful completion of the process, the Catchment grid “Cat” is added to the map. You can recolor the grid with
unique values to get a nice display.
Confirm that the input to the Catchment Grid is “Cat”. The output is the Catchment polygon feature class, having the default name
“Catchment” that can be overwritten.
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Press OK. Upon successful completion of the process, the polygon feature class “Catchment” is added to the map.
Open the attribute table of "Catchment". Notice that each catchment has a HydroID assigned that is the unique identifier of each
catchment within ArcHydro. Each catchment also has Shape Length and Area attributes. These quantities are automatically computed
when a feature class becomes part of a geodatabase.
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Confirm that the input to Link Grid is “Lnk” and to Flow Direction Grid “Fdr”. The output Drainage Line has the default name
“DrainageLine” that can be overwritten.
Press OK. Upon successful completion of the process, the linear feature class “DrainageLine” is added to the map.
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Step 2: Select the “DrainageLine” Shapefile in the first pull down menu.
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Step 3: In the Second pull down menu, Browse the Output location to Store KML file and give the name “Drainage”.
Step 4: In the Third pull down menu, give output scale 50,000.
Step 5: Click Ok. After completing the process, open “Drainage.kmz” in Google earth.
6. Tutorial
1. Cell size, Number of rows and columns of DEM, maximum and minimum elevation values in Himachal.tif.
3. Perform same exercise with 500 thresholds and calculate number of catchment.
4. Make a screen capture of the attribute table of Fdr and give an interpretation for the values in the Value field using a sketch.
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