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Hydrological modeling of the Congo River basin: Asoil-water balance approach

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par Bahati Chishugi Josue
University of Botswana - Masters of Sciences (M.Sc.) 2008
  

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CHAPTER FOUR

4.0 METHODOLOGY

The present chapter comprises two major sections describing the watershed and streams characteristics method of determination and the water balance modelling method.

4.1 Watershed and streams characteristics

The concept of a watershed is basic to all hydrologic designs. Watershed has been defined as an area of land draining into a stream at a given location (Chow et al, 1988). In other words and usually a watershed is defined as the area that appears, on the basis of topography, to contribute all the water that passes through a given cross section of a stream. The surface trace of the boundary that delimits a watershed is called a divide, and the horizontal projection of the area of a watershed is called the drainage area of a stream at that cross section, while the location of the stream cross section that defines the watershed is determined by the analysis.

Since large watersheds are made up of many smaller watersheds, it is necessary to define the watershed in terms of a point. This point is usually the location at which the design is being made and is referred to as the watershed «outlet». With respect to the outlet, the watershed consists of all land area that «sheds» water to the outlet during a rainstorm. Using the concept that «water runs downhill», a watershed is defined by all points enclosed within an area from which rain falling at these points will contribute water to the outlet (McCuen, 2005).

To delineate the Congo River Watershed and streams network, a Digital Elevation Model (DEM), HYDRO 1K with 1 km of spatial resolution, later on described, was used and processed with Geographical Information System packages viz Integrated Land and Water System (ILWIS) and ArcGIS.

In the following section are presented different steps followed for the DEM-Hydro watershed processing. The purpose of this chapter is to define and hydrogeomorphologically charcterise the watershed and streams behaviours of the Congo basin, availing useful data sets for hydrological modellings.

4.2 Watershed and drainage network Processing Method

The detailed processing method presented bellow (Figure 12) is a combination of techniques used in GIS ILWIS 3.4, ArcINFO 9.2 and ArcView 3.2 packages; it consists in:

1 DEM visualization

2 Flow Determination (Fill sinks, Flow direction, Flow accumulation, Flow

Modification)

3 Variable threshold computation

4 Network and Catchment Extraction (Drainage network extraction, Drainage

network ordering, Catchment extraction, Catchment merge

5 Compound Parameter Extraction (Overland flow length, Compound Index

calculation)

6 Statistical Parameter Extraction (Horton statistics, aggregate statistics, cumulative

hypsometric curve, class coverage).

DEM
1 kHYDRO 30sec

Statatistical Parameters Extraction

HORTON statistics

Cumulative Hypsometric Curve

Threshold

Outlets coordinate

Digitized Drainage

Minimum Drainage Length

Compound Parameters Extraction

Drainage Network Ordering

Catchment Extraction

Catchment Merge

Drainage Network Extraction

DEM Optm

DEM Fill Sinks

Flow Direc

Flow Accu

Drainage Network Ordering Map

DEM Optm Map

DEM Filled Map

Flow Direct Map

Flow Accu Map

Drainage Map

Overland Flow length Map

Catchment Maps

Extract Stream Segments + Attributes

Wetness/Power/Sediment indexes Maps

Catchment Merged Map

Longest Flow Path Segment Map

Figure 12 DEM Processing flow chart: Extraction of Drainage network, Catchment and Horton Parameters.

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