Versions Compared

Key

  • This line was added.
  • This line was removed.
  • Formatting was changed.

...

CUBE algorithm is highly recommended to produce bathymetry surface unless it is not possible/available. When generating bathymetric surfaces, seabed depths dictate the grid resolution. Grid resolution is determined by AusSeabed depth bands (Table 3). Typically, a single grid is made for a survey, but we also accept multiple grids. It is required that the bathymetry grid(s) extends from the start and end port of the survey (port to port).

 

Table 39. AusSeabed depth bands and associated grid resolutions. Modified from NOAA (2019)

Normal depth band (≤45°)

Steep slope depth band (>45°)1

Res (m)

Ratio2

Ds (m)

Dd (m)

Range Interval (m)

Ds (m)

Dd (m)

Range Interval (m)

0

20

20

0

20

20

0.5

0.0250

18

40

22

16

40

24

1

0.0250

36

80

44

32

80

48

2

0.0250

72

160

88

64

160

96

4

0.0250

144

320

176

128

320

192

8

0.0250

288

640

352

256

640

384

16

0.0250

576

1280

704

512

1280

768

32

0.0250

1152

2560

1408

1024

2560

1536

64

0.0250

2304

5120

2816

2048

5120

3072

128

0.0250

4608

12000

7392

4096

12000

7904

210

0.01753

1In cases of steep slopes, the overlap between grids of different resolutions may need to be increased to prevent gaps in their junction. In these cases, the coarser resolution grid should have its shoaler extent modified to prevent this coverage gap. 2Highest resolution at which the dataset can support a minimum of five soundings per node (ideally, twice the maximum standard required survey resolution for the depth of the area, i.e. 2.5% water depth) (NOAA, 2019). 3Based on 1⁰ beamwidth (highest resolution that the current technology of shipborne systems can effort) because of the constraint in the minimum capture distance in CUBE to a maximum of 100.

...