This ILWIS User’s Guide has been rewritten and extended by Raymond Nijmeijer Figure The process of tunneling using two different tunnel widths. Today I’ll start with a new series of tutorials for an open Source GIS called “ILWIS GIS“. ILWIS is the short term for “Integrated Land and Water. A complete package: ○ image processing. ○ spatial analysis. ○ digital mapping . ○ Easy to learn and use: ○ full on-line help. ○ extensive tutorials for direct.

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More information on the operation can be found at the Drainage Network Ordering webpage. This can be seen in Figure This operation is commonly used to determine potential drainage patterns of terrain. Retrieved from ” https: Keeping all your data in one folder will make analysis easier.

Exploring Hydrological Analyses using ILWIS – CUOSG

Flow direction depicts a main direction of flow run-off. In order to carry out this exercise, a DEM of the area of interest is needed. The table lists all the streams with ID values, coordinates, lengths, slope of drainage. Fills should be run on DEMs to remove any local depressions, which can cause inaccuracies in following hydrological analyses.

This will create a map showing the distance a flow must travel to reach the outlet of a given watershed. Navigation Main page Recent changes Random page Help. The flow length value in metres will appear in the table on the bottom left portion of the screen. The map is boolean and will illustrate the drainage as pixels tuttorial value True, while all other pixels have value of False.

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In the future, newer tuorial may also be possible, but the tutorial will need to be verified on them. Output consists of both a map and a Table.

This tutorial covers the most basic hydrological tools for a more simple and basic hydrological analysis using ILWIS. Drainage Network Extraction extracts a drainage network map. Under Save as browse to the desired folder location for your projected DEM and rename it.

Overland Flow Length overland distance towards the ‘nearest’ drainage for each tutoriak based on flow paths available from the Flow Direction Map.

The output map will show the different sub watershed and the flow length ilis each cell to reach the outlet. Operations that have not been covered but should be considered when desiring a more in-depth and accurate analysis include:. For a more in-depth analysis look into the topics not covered in this tutorial.

The objective ikwis this tutorial is to provide users with a better understanding of how the hydrological analyses within ILWIS works, in addition to providing the instructions necessary to reach the desired output for their study region.

The pixel value is determined by the Flow Accumulation Map and a threshold value.

Flow Accumulation is calculated from the map created in Flow Direction, counting the number of cells that would drain into outlets based on the flow direciton. You will have to navigate to the working folder and select the DEM.

More information on the operation can be found at the Drainage Network Extraction webpage. The flow direction operation determines into which neighbouring pixel any water from a given pixel would flow.

Digital Geography

Drainage Network Ordering operation finds all drainage line in the Drainage Network and their nodes, and applies a unique ID to each stream. This can be downloaded from the QGIS website. To determine the flow length of a specific cell, use the normal mouse cursor and click on the area of interest.


Before starting any analysis, create your working folder and ensure all data needed for the exercise are in this folder. This tutorial will focus on its ability to use Digital Elevation Models DEMs to run hydrological liwis of a study region. The threshold value in this operation is the minimum value required for a flow to be considered True in a drainage network, all cells with a value lower than the threshold will be classified as False.

Exploring Hydrological Analyses using ILWIS

This project will focus on hydrological analysis of Okanagan Lake, a popular tourist destination in British Columbia, Canada. This is determined by a moving 3×3 window for every single pixel, based on its neighbouring pixels height values.

Flow Accumulation performs a cumulative count of the number of pixels that would flow into any given cell on the ttuorial to an outlet. It is an open source Geographic Information System software program that was designed to be a user-friendly integrated software that contains both raster and vector processing capabilities, allowing for both analyses on remotely sensed images, vector maps and numerous spatial modeling abilities.

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