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The Data menu provides options for bathymetry interpolation as well as accessing online bathymetry data. Being able to view bathymetry underneath the grid helps determine the resolution required in the deep and main channel regions compared to shallow regions, which can often have lower resolutions. The Grid Bathymetry Interpolation and Download Online Bathymetry options are shown in Figure 1 and their use is described below.

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From the Import button in the main toolbar, select Import Cross-Sections option, as shown in Figure 3. The Import Cross-Sections form will be displayed. Browse to the cross-section file, then click the Open button (Figure 4), as a result, cross-sections are displayed as shown in Figure 5.

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Figure 3
Figure 3

Figure 3 Import cross-sections option.

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Figure 4 Import cross-section file.

The Coordinate System form will pop up. We need to select proper projection for the imported cross sections as shown in Figure 5 then click OK button, as the result, the cross-sections will be displayed as shown in Figure 6.

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Figure 5
Figure 5

Figure 4 Import cross-section file.5 Define projection.


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Figure 6
Figure 6

Figure Cross-sections loaded.

To display the elevation of the cross-sections by color ramp, press Alt+C from the keyboard, and the Specify Elevation will pop up. Enter the Min and Max values for the elevation range (this range is based on the Z column value in the cross-section file). In this case, enter 0, -15 (Figure 67). Then click the OK button, and the cross-section will be displayed as shown in Figure 78.

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Figure 67
Figure 67


Figure Cross-sections loaded.

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Figure 78
Figure 78


Figure Cross-sections displayed in color ramp.

Grid Bathymetry Interpolation for Dense Cross-Sections

For the river segment, the available cross-sections are dense, so it is possible to interpolate grid bathymetry directly. First, draw a grid for the selected river segment, it is advised to create a fine grid to advance the interpolation results. Then, select the grid layer in the Layer Control panel, and select Grid Bathymetry Interpolation option from the Data menu as shown in Figure 8Suppose that a gird that covers the cross-sections is available. Now load the grid, then we are going to interpolate its bathymetry.

Go to the Data menu, then select Grid Bathymetry Interpolation as shown in Figure 9. The Topographic Interpolation form will be displayed pop up as shown in Figure 910.

  • Grid Layer : is the name of the selected grid layer that we are going to will interpolate its bathymetry.
  • Using Visible Data: is the number of data points. In this case, there are 2234 points from the cross-section file.
  • Interpolation Options: There are two options, including Update Missing Only (update elevation values for the missing grid nodes only, in case other nodes already have elevation values) and Overwrite All Data (create new elevation values for all grid nodes and overwrite the nodes that have existing elevation values).
  • Interpolation MethodGrid+ currently uses only one interpolation method, the Inverse the Inverse Distance Weighting (IDW) is used. The IDW Options frame allows changing its properties.

Click the Interpolate button to

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proceed interpolation process, when it is done, click the OK button to close the form.

After the interpolation process is done, RMC on the grid layer and select Show Properties / Bottom Elevation to display the bottom elevation of the grid after its grid nodes are assigned elevation values, as shown in Figure 1011.

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titleNote

The bottom elevation values for the grid are for grid nodes, not for the centroid of grid cells.


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Figure 89
Figure 89


Figure Grid Bathymetry Interpolation.

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Figure 910
Figure 910

Figure 10  Topographic Interpolation form.

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Figure 1011
Figure 1011

Figure 10  11  Grid with bottom elevation.

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Select the Add a new polyline button from the main toolbar, then start drawing a polygon that covers the grid as shown in Figure 1112. Change the cursor to select object mode (press the S key or select the Select Object in the main toolbar). Select the overlay layer (the layer that contains the polygon), then LMC on the polygon (it will be highlighted by changing color to red), then RMC to display options, and select the Interpolate Grid Elevations option as shown in Figure 1213. A message will be shown as in Figure 1314 when the interpolation process is complete. Click the OK button to close the message.

RMC on the grid layer and select Show Properties / Bottom Elevation to display the bottom elevation of the grid after its grid nodes are assigned elevation values, as shown in 2127790207 Figure 15.

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Figure 1112
Figure 1112

Figure 11  12  Draw a polygon that covers the grid.


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Figure 1213
Figure 1213

Figure 12  13  Interpolation by using a polygon.


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Figure 1314
Figure 1314

Figure 13  14  Grid Bathymetry Interpolation message.

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Figure 1415
Figure 1415

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Figure 14  15  Grid with bottom elevation(2).

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In reality, the available the other case, there are few cross-sections in some river segments are few ( as the example in Figure 15). Therefore, Grid+ support interpolates grid bathymetry by blocks and then extends to the entire grid. Firstly, draw a fine grid to cover the cross-section as shown in Figure 16. Then draw , and they are far from each other. Apply the Inverse Distance Weighting (IDW) interpolation method as the previous introduction is not proper. The following section describes other interpolation methods.

Suppose that there are two cross-sections loaded as shown in Figure 16.. Next, generate a grid that covers the two cross-sections. Note that the grid should have high resolution (grid cells).

The grid is displayed as shown in Figure 17. We can see that only some grid cells in two head ends of the grid cover the cross sections. We should interpolate for those cell's bathymetry first.

Draw a polygon to cover the grid cells near the available cross-section sections.

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Figure 1516
Figure 1516

Figure 15  Sparse cross16  Cross-sections loaded and located in the river segment.

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Figure 1617
Figure 1617

Figure 16  Grid to cover 17 High-resolution grid covers the cross-sections.

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Figure 18
Figure 18

Figure 17  Grid to cover the 18  Draw two polygons covering grid cells and cross-sectionssection.








Download Online Bathymetry

After selecting the Download Online Bathymetry option, the Download Online Data form will be displayed as shown in 2127790207. Users are able to select data set using the drop-down Data Set. The currently available open-source sites are:

  • GEBCO 2021: This is 2021 GEBCO’s gridded bathymetric data set, the GEBCO_2021 Grid, is a global terrain model for ocean and land, providing elevation data, in meters, on a 15 arc-second interval grid. The data information can be found on GEBCO's website GEBCO 2021.
  • GEBCO 2014: This is 2014 GEBCO’s gridded bathymetric data set. The data information can be found on GEBCO's website GEBCO 2014.
  • GEBCO 08: a continuous terrain model for ocean and land with a spatial resolution of 30 arc-seconds released by the General Bathymetric Chart of the Oceans (GEBCO) in 2009. Bathymetric data is available to download, and the user manual can be found on the website GEBCO 08.

Depending on the data set selected, different data information is provided in the Spatial Information section. The Data Extraction Limits is auto-set to the whole model domain, but the user can manually select the specific area by checking to Using Polygon File and browser to the closed polygon that contains the area inside.

Click on Download button and Grid+ will download and apply the bathymetry data of the selected Data Set to the specific defined area.

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Figure 15
Figure 15


Figure 15  Download online data for bathymetry.

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