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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.  In many cases, bathymetry data needs to be interpolated to cover the whole domain. This section describes features unique to Grid+ whereby a user may interpolate between two cross-sections along even over a sinusoidal domain.  The Grid Bathymetry Interpolation and Download Online Bathymetry options are shown in Figure 1 and their use is described below.

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Figure 1
Figure 1


Figure 1. Data menu options.

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Simple Interpolation of Grid Bathymetry

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In cases where cross-section data is available, it can be viewed in Grid+ with files in ldb format. For example, a file with name XS.ldb contains cross-sections with the following information (Figure 2).

  • The first row is the name of the cross-section.
  • The second row has a contains the number of data points (e.g 11), and a the number of columns (e.g 3) of for each data point. It This includes coordinates (X, Y) and Z (elevation)
  • Data points start from the third row to end.

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Figure 2
Figure 2


Figure 2. Cross-section data format.

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 Data Menu#Data Menu#Figure 4).

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Figure 3
Figure 3

Figure 3. Import cross-sections option.

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Figure 4
Figure 4

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 Data Menu#Data Menu#Figure 5. Click the OK button , as and the result, the cross-sections will be displayed as shown in Figure Data Menu#Data Menu#Figure 6.

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Figure 5
Figure 5

Figure 5. Define projection.


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Figure 6
Figure 6

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Figure 6. 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 Data Menu#Data Menu#Figure 7). Then click the OK button, and the cross-section will be displayed as shown in Figure Data Menu#Data Menu#Figure 8.

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Figure 7
Figure 7


Figure 7. Cross-sections loaded.

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Figure 8
Figure 8

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Figure 8. Cross-sections displayed in color ramp.

Suppose that a gird In cases where a grid that covers the cross-sections is available . Now we can load the grid , then we are going to interpolate its bathymetry onto it.

Go to the Data menu, then select Grid Bathymetry Interpolation as shown in Figure Data Menu#Data Menu#Figure 9. The Topographic Interpolation form will pop up as shown in Figure Data Menu#Data Menu#Figure 10.

  • Grid Layer : is the name of the selected grid layer for which we will interpolate its the bathymetry.
  • Using Visible Data: is the number of data points. In this case, there are 2234 points from in 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 Method: Inverse Distance Weighting (IDW) is used. The IDW Options frame allows changing its of the interpolation properties.

Click the Interpolate button to proceed with the interpolation process. When it is donecomplete, click the OK button to close the form.

After the interpolation process is donecomplete, 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 Data Menu#Data Menu#Figure 11.

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


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Figure 9
Figure 9

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Figure 9. Grid Bathymetry Interpolation.

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Figure 10
Figure 10

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Figure 10  10. Topographic Interpolation form.

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Figure 11
Figure 11

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Figure 11  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 Data Menu#Data Menu#Figure 12. 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 Data Menu#Data Menu#Figure 13. A message will be shown as in Figure Data Menu#Data Menu#Figure 14 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 Figure Data Menu#Data Menu#Figure 15.

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Figure 12
Figure 12

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Figure 12  12. Draw a polygon that covers the grid.


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Figure 13
Figure 13

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Figure 13  13. Interpolation by using a polygon.

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Figure 14
Figure 14

Figure 14  14. Grid Bathymetry Interpolation message.

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Figure 15
Figure 15


Figure 15  15. Grid with bottom elevation(2).

Other Interpolation Methods

In the other second case, we will look at there are few cross-sections, and they are far apart from each other. Apply the The Inverse Distance Weighting (IDW) interpolation method as used in the previous introduction is not proper. The following section describes other interpolation methodsan appropriate approach. Instead, interpolation using an orthogonal curvilinear grid will be used in this case.

Suppose that there are two cross-sections loaded as shown in Figure Data Menu#Data Menu#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 Data Menu#Data Menu#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 the bathymetry of those cells first.

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Figure 16
Figure 16

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Figure 16. Cross-sections loaded and located in the river segment.

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Figure 17
Figure 17

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Figure 17. High-resolution grid covers the cross-sections.


Click Add a polyline button from the Main Toolbar to draw a polygon to cover the grid cells near the cross-sections, as shown in Figure Data Menu#Data Menu#Figure 18. Then, 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 new polygon), then LMC on the polygon to select it (it will be highlighted by changing its color to red), then RMC to display options, and select the Interpolate Grid Elevations option as shown in Figure Data Menu#Data Menu#Figure 19. A message will be shown as in Figure Data Menu#Data Menu#Figure 20 when the interpolation process is complete. Click the OK button to close the message.

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Apply similar steps to interpolate the bottom elevation of grid cells near the second cross-section.

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Figure 18
Figure 18

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Figure 18. Draw two polygons covering grid cells and cross-section.

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Figure 19
Figure 19

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Figure 19. Interpolate grid cells near the cross-section.

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Figure 20
Figure 20

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Figure 20. Grid Bathymetry Interpolation message.


To view the bottom elevation of cells that are interpolated, RMC on the grid layer and select Show Properties / Bottom Elevation as shown in Data Menu#Data Menu#Figure 21. The grid bottom elevation will be displayed as shown in Data Menu#Data Menu#Figure 22.

Next, we will interpolate the bottom elevation for the entire

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grid based on the cells with the existing bottom elevation in two ends of the grid. Select the grid layer in the

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Control Panel and

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set the cursor

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in selection mode. Select the

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first grid node

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and hold the Shift key to select the second node

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(select two grid nodes to define the grid block we want to interpolate). In this case, we select two grid nodes to cover the entire grid. The grid block will be highlighted by changing the color to red

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, then RMC to display options

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and select the Interpolate Elevations in I Direction option as shown in 

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Data Menu#Data Menu#Figure 23.

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After the interpolation process is done,  the grid bottom elevation

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Figure 16  Cross-sections loaded and located in the river segment.

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Figure 17 High-resolution grid covers the cross-sections.

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Figure 18  Draw two polygons covering grid cells and cross-section.

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Figure 19  Interpolate grid cells near the cross-section.

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Figure 20  Grid Bathymetry Interpolation message.

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is displayed as shown in Data Menu#Data Menu#Figure 24.

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Figure 21
Figure 21

Figure 21  21. Show the grid bottom elevation of grid cells.

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Figure 22
Figure 22

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Figure 22  22. Grids with bottom elevation at two cross-sections.

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Figure 23
Figure 23

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Figure 23  23. Interpolate the grid block in I direction.

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Figure 24
Figure 24

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Figure 24  24. Grid with bottom elevation.

Extrapolation of Bathymetry

Besides this interpolation feature, Grid+ has a feature to replicate the grid elevation. For example, in an extrapolation feature. In this case, some upper grid cells cells in the two ends of the grid are missing the data of bottom elevation. FirstlyTo fill in their bottom elevation, select the grid layer in the control panel Control Panel and change set the cursor to in selection mode. Select a grid node and hold the Shift key to select the second node, the block that covers both cells missing bottom elevation and cells having bottom elevation. The grid block will be highlighted by changing the color to red. Note that the number of grid cells having bottom elevation values should be similar to the cells missing data. Then RMC to the grid cells to display options , and select the Extend Elevations in I Direction option as shown in Figure Data Menu#Data Menu#Figure 25. The bottom elevation values will be expanded extended to the upper cells Figure 26 presents the grid bottom elevation after extensionthat are missing values. As a result, the bottom elevation for those cells is assigned as shown in Data Menu#Data Menu#Figure 26.

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Figure 25
Figure 25

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Figure 25  25. Extend elevation in I-direction.

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Figure 26
Figure 26

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Figure 26  26. Grid cells after extension bottom elevation.


Exporting to a Scatter Data File

After interpolating the bathymetry of the grid cells, Grid+ allows exporting the bathymetry to a scatter data file. To do this, RMC on grid layer, then select Create Scatter Data from Elevation option as shown in Data Menu#Data Menu#Figure 27. This will extract the grid node’s elevation and then create an XYZ scatter layer in the Layer Control. It is named  “XYZ from Grid”. RMC on XYZ from Grid layer, select Export Data Point ( as shown in Data Menu#Data Menu#Figure 28) and browse to the location to save the file, enter a file name, then click OK button to export the layer to a file.

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Figure 27

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Figure 27. Create scatter data from elevation.

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Figure 28
Figure 28

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Figure 28. Export bottom elevation to data file.

Download Online Bathymetry

After selecting the Download Online Bathymetry option, the Download Online Data form will be displayed as shown in Figure 2729. 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 2729
Figure 2729


Figure 27  29. Download online data for bathymetry.

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