Abstract:
A watershed is the upslope area that contributes flow generally water to a common outlet as concentrated drainage. It can be part of a larger watershed and can also contain smaller watersheds, called sub-basins. The boundaries between watersheds are termed drainage divides. The outlet, or pour point, is the point on the surface at which water flows out of an area. It is the lowest point along the boundary of a watershed.
In the present study watershed in Satara district of Maharashtra is used for various urban planning work. Geographical Information Systems (GIS) and a high-resolution Digital Elevation Model (DEM) has been utilized for the estimation of watershed. Several hydrological parameters have been computed such as flow direction, flow accumulation, stream order, watershed etc.
Key words: Digital Elevation Model, GIS, Remote Sensing, Satara watershed, Urban Planning
Introduction
Watershed delineation is a crucial process in urban area planning, as it provides an understanding of how water flows through a given landscape, from its highest points to its outlets. A watershed, also known as a drainage basin, is the geographic area that collects rainwater and directs it to a common outlet such as a river, lake, or storm drain. In the context of urban planning, delineating watersheds is essential for managing storm water, preventing floods, and ensuring sustainable development.
Urbanization significantly alters natural hydrological processes. The increase in impervious surfaces like roads, buildings, and parking lots reduces natural infiltration, increasing surface runoff and the risk of flooding. By delineating watersheds, planners can assess how water will flow and accumulate in urban environments, helping to inform critical infrastructure decisions, storm water management, and environmental conservation strategies.
Delineating watersheds helps planners and engineers to:
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Manage Storm water: Properly designed storm water systems, including retention basins, drainage networks, and green infrastructure, rely on watershed analysis to control and manage runoff.
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Mitigate Flood Risks: Identifying flood-prone areas within a watershed helps in the implementation of flood control measures, zoning regulations, and resilient infrastructure design.
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Sustainable Urban Growth: By understanding the flow of water within a watershed, urban planners can develop land-use plans that protect natural resources, reduce erosion, and enhance groundwater recharge.
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Enhance Climate Resilience: Watershed data enables cities to prepare for the effects of climate change, such as increased rainfall and flooding, by guiding adaptive measures and resilient urban design.
Incorporating watershed analysis into urban planning not only enhances the sustainability of urban environments but also improves the safety and quality of life for urban populations by managing water resources effectively.
Study Area: Satara
Satara district is situated in the river basins of the Bhima and Krishna river. The physical settings of Satara show a contrast of immense dimensions and reveal a variety of landscapes influenced by relief,climate and vegetation. The variation in relief ranges from the pinnacles and high plateaus of main Sahyadrians range having height over 4500 feet above mean sea level to the subdued basin of the Nira river in Phaltan tehsil with the average height of about 1700 feet above mean sea level. The climate ranges from the rainiest in the Mahabaleshwar region, which has an average annual fall of over 6000 mm to the driest in Man tehsil where the average annual rainfall is about 500 mm. The vegetal cover too varies from the typical monsoon forest in the western parts to scrub and poor grass in the eastern parts.
Geographical location: North Latitudes 17.5 to 18.11 : East Longitude 73.33 to 74.54
Geographical Area: 10480 (sq.km.)
The main rivers of Satara district are Koyna and Krishna. The Krishna is one of the three largest sacred rivers of southern India. Approx. 172 kms.of the river course falls inside the district. The Krishna river begins on the eastern brow of the Mahabaleshwar plateau and the source is about 4500 ft. above sea level.
Kudali, Urmodi, Venna and Tarali are small feeder rivers of Krishna. Koyna is the largest tributary of Krishna in the district. Neera and Manganga rivers are the two representatives of the Bhima drainage in the north and north-eastern parts of the district respectively. The Satara district in Maharashtra, India has several watersheds, including the Urmodi River
watershed and the Mahabaleshwar-Koyna watershed region:
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Urmodi River watershed: A tropical watershed located in the Satara district
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Mahabaleshwar-Koyna watershed region: A region that includes hill stations and holiday places, such as Mahabaleshwar and Panchgani
[Figure1. Showing Study area Satara]
Methodology:
Delineating a watershed using Digital Elevation Model (DEM) data in ArcGIS Pro is a step-by-step process that involves terrain analysis and the use of hydrology tools to define the boundaries of a watershed.
Below is a detailed guide on how to do this:
Steps to Delineate a Watershed Using DEM in ArcGIS Pro:
1. Prepare DEM Data:
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Acquire DEM: Ensure you have a DEM for the study area. This can be downloaded from sources such as the USGS (for the US), NASA SRTM, or your local government’s geospatial data portal.
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Load DEM into ArcGIS Pro: Open ArcGIS Pro and add the DEM to the map by dragging it into the contents pane.
2. Fill Sinks in the DEM:
Sinks (depressions in the DEM) can create problems when calculating flow direction. The first step is to fill these sinks to create a smooth surface.
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Go to the Geoprocessing Pane and search for the Fill tool.
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Input your DEM as the "Input Surface Raster.
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Run the tool to fill sinks and create a smoothed DEM.
3. Generate Flow Direction:
The next step is to calculate the direction in which water will flow across the surface, based on the filled DEM.
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Search for the Flow Direction tool in the Geoprocessing Pane.
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Set the "Input Surface Raster" to the filled DEM from the previous step.
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Run the tool to generate the flow direction raster.
4. Create Flow Accumulation:
This step calculates the accumulated flow to each cell in the raster based on the flow direction, helping identify potential stream networks.
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In the Geoprocessing Pane, search for the Flow Accumulation tool.
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Input the flow direction raster as the "Input Flow Direction Raster."
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Run the tool to produce a flow accumulation raster.
5. Identify Streams:
To create a stream network, you need to determine which areas have enough accumulated flow to form streams.
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Use the Raster Calculator tool to apply a threshold to the flow accumulation raster. A higher threshold results in fewer, larger streams, while a lower threshold produces more streams.
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Formula: "Flow Accumulation Raster" > threshold_value
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Choose a threshold value based on the scale of your analysis (e.g., 1000 or 5000).
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Run the calculation to get a binary stream network (1 for streams and 0 for non stream cells).
6. Define the Pour Point (Outlet):
The pour point is where water exits the watershed, such as at a river mouth or a designated point on a stream. You can manually create pour points or use existing stream data:
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Add a point feature at the outlet location (the lowest point or where you want to delineate the watershed).
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Snap this point to the nearest stream to ensure accurate watershed delineation.
7. Snap Pour Point to Flow Accumulation:
Ensure the pour point aligns with the highest flow accumulation in its vicinity.
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Use the Snap Pour Point tool:
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Input the pour point feature and the flow accumulation raster.
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Set a snap distance (within which the point will snap to the highest flow accumulation pixel).
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Run the tool to snap the pour point to the nearest high-flow area.
8. Delineate the Watershed:
With the pour point defined, the watershed can be delineated based on the flow direction raster.
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Search for the Watershed tool in the Geoprocessing Pane.
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Set the "Input Flow Direction Raster" to the flow direction raster and "Input Pour Point Data" to the snapped pour point feature.
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Run the tool to delineate the watershed. This will generate a raster representing the watershed area draining to the pour point.
9. Convert Watershed Raster to Polygon:
To make the watershed more manageable for analysis and visualization, convert the raster to a polygon.
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Use the Raster to Polygon tool to convert the watershed raster into a vector format.
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Input the watershed raster and select "Simplify Polygon" to clean up the boundaries.
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Run the tool to create a watershed polygon.
10. Visualize and Analyze the Watershed:
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Symbolize the watershed polygon to distinguish it from other features in the map.
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You can overlay the watershed boundary with other spatial data, such as land use, land cover, or urban infrastructure, to begin your analysis.
By following these steps, you can effectively delineate a watershed using DEM data in ArcGIS Pro, providing the foundation for various environmental, hydrological, and urban planning applications.